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The paleo-tectonic maps of retired geologist Ronald Blakey are mesmerizing and impossible to forget once you've seen them. Catalogued on his website Colorado Plateau Geosystems, these maps show the world adrift, its landscapes breaking apart and reconnecting again in entirely new forms, where continents are as temporary as the island chains that regularly smash together to create them, on a timescale where even oceans that exist for tens of millions of years can disappear leaving only the subtlest of geological traces.

With a particular emphasis on North America and the U.S. Southwest—where Blakey still lives, in Flagstaff, Arizona—these visually engaging reconstructions of the Earth's distant past show how dynamic a planet we live on, and imply yet more, unrecognizable changes ahead.

The following images come from Ron Blakey's maps of the paleotectonic evolution of North America. The first map shows the land 510 million years ago, progressing from there—reading left to right, top to bottom—through the accretion and dissolution of Pangaea into the most recent Ice Age and, in the final image, North America in its present-day configuration.



Venue met with Blakey in his Flagstaff home to talk about the tectonic processes that make and remake the surface of the Earth, the difficulty in representing these changes with both scientific accuracy and visual panache, and the specific satellite images and software tools he uses to create his unique brand of deep-time cartography.

Like film stills from a 600-million year-old blockbuster, Blakey's maps take us back to the Precambrian—but there are much older eras still, stretching unmapped into far earlier continents and seas, and there are many more billions of years of continental evolution to come. Blakey talked us through some of the most complex changes in recent geological history, including the opening of the North Atlantic Ocean, and he allowed himself to speculate, albeit briefly, about where Earth's continental crust might yet be headed (including a possible supercontinent in the Antarctic).

Many of Blakey's maps are collected in the book Ancient Landscapes of the Colorado Plateau, written with Wayne Ranney, where Blakey also describes some of the research and methods that went into producing them. Blakey also contributed to the recent, new edition of a textbook by Wolfgang Frisch and Martin Meschede, Plate Tectonics: Continental Drift and Mountain Building, a thorough exploration of landscapes disassembling and colliding over vast spans of time.

• • •

The west coast of North America, depicted as it would have been 130 million years ago; the coast is a labyrinth of islands, lagoons, and peninsulas slowly colliding with the mainland to form the mountains and valleys we know today. Map by Ron Blakey.

Geoff Manaugh: When I first discovered your maps showing the gradual tectonic re-location of the continents over hundreds of millions of years, I thought this was exactly what geologists should be doing: offering clear, step-by-step visual narratives of the evolution of the earth’s surface so that people can better understand the planet we live on. What inspired you to make the maps, and how did you first got started with them?

Ronald Blakey: Well, the very first maps I made were in conjunction with my doctoral thesis, back in the early 1970s. Those were made with pen and ink. I made sketches to show what the paleogeography would have looked like for the specific formation I was studying with my doctorate. Three or four of those maps went into the thesis, which was then published by the Utah Geologic Survey. I’ve also done a number of papers over the years where I’ve made sketches.

But I was late getting into the computer. Basically, during my graduate work I never used a computer for anything. I kind of resisted it, because, for the kind of work I was doing, I just didn’t see a need for it—I didn’t do quantifiable kinds of things. Then, of course, along comes email and the Internet. I actually forget when I first started with Photoshop—probably in the mid-1990s. When I found that, I just thought, wow: the power of this is incredible. I quickly learned how to use the cloning tool, so that I could clone modern topography onto ancient maps, and that made things even simpler yet.

Another thing I started doing was putting these maps into presentations. There were something like five different programs back there, in the late 90s, but the only one that survived was PowerPoint—which is too bad, because it was far from the best of the programs. I was using a program called Astound, which was far superior, particularly in the transitions between screens. I could do simple animations. I could make the tectonic plates move, create mountain belts, and so forth.

I retired in May of 2009, but all of my early maps are now online. With each generation of maps that I’ve done, there has been a noted improvement over earlier maps. I find new techniques and, when you work with Photoshop as much as I do, you learn new ideas and you find ways to make things that were a little clumsy look more smooth.

Manaugh: Where does the data come from?

Blakey: It comes from various publications. You can get a publication and have that PDF open, showing what something looked like in the past, and work from that. Usually, what I’m working from are fairly simple sketches published in the literature. They’ll show a subduction zone and a series of violent arcs, or a collision zone. What I do is take this information and make it more pictorial.

If you create a series of maps in sequence, you can create them in such a way that certain geologic events, from one time slice to the next, to the next, to the next, will blend. It depends a lot on the scale of what you’re trying to show—the whole world versus just four or five states in the West.

Now, throughout the years from, let’s say, 2004 until I retired in 2009, I kept improving the website. I envisioned most of this as educational material, and I didn’t pay much attention to who used it, how they used it, and so forth. But, then, shortly before I retired, various book companies and museums—and, most recently, oil companies—have approached me. So I started selling these and I tried very diligently not to allow this to overlap with what I was doing for my teaching and my research at the University.

In the following long sequence of images, we see the evolution of the west coast of North America, its state boundaries ghosted in for reference. Sea levels rise and fall; island chains emerge and collide; mountains forms; inland seas proliferate and drain; and, eventually, modern day California, Vancouver Island, and the Baja peninsula take shape, among other recognizable features. The time frame represented by these images is approximately 500 million years. All maps by Ron Blakey.



Nicola Twilley: What do the oil companies want them for?

Blakey: They’re my biggest customers now. Usually, the geologists at oil companies are working with people who know either much less geology than they do or, in some cases, almost no geology at all, yet they’re trying to convince these people that this is where they need to explore, or this is what they need to do next.

They find these maps very useful to show what the Devonian of North Dakota looked like, for example, which is a hot spot right now with all the shales that they’re developing in the Williston Basin. What they like is that I show what the area might have really looked like. This helps, particularly with people who have only a modest understanding of geology, particularly the geologic past.

Manaugh: What have been some of the most difficult regions or geological eras to map?

Blakey: The most difficult thing to depict is back in the Paleozoic and the Mesozoic. Large areas of the continent were flooded, deep into the interior.

During certain periods, like the Ordovician, the Devonian, and parts of the Jurassic—especially the Cretaceous—as much as two-thirds of the continents were underwater. But they’re still continents; they’re still continental crusts. They’re not oceans. The sea level was just high enough, with respect to where the landscape was at the time, that the area was flooded. Of course, this is a concept that non-geologists really have problems with, because they don’t understand the processes of how continents get uplifted and subside and erode and so forth, but this is one of the concepts that my maps show quite nicely: the seas coming in and retreating.

But it’s very difficult—I mean, there is no modern analog for a seaway that stretched from the Mackenzie River Delta in Canada to the Gulf of Mexico and that was 400 miles wide. There’s nothing like that on Earth today. But the styles of mountains have not dramatically changed over the last probably two billion years—maybe even longer than that. I don’t go back that far—I tend to stick with the last 600 million years or so—but the styles of mountains haven’t changed. The nature of island arcs hasn’t changed, as far as we know.

What has changed is the amount of vegetation on the landscape. My maps that are in the early part of the Paleozoic—the Cambrian and the Ordovician early part of the Silurian—tend to be drab-colored. Then, in the late Silurian and in the Devonian, when the land plants developed, I start bringing vegetation colors in. I try to show the broad patterns of climate. Not in detail, of course—there’s a lot of controversy about certain paleoclimates. But, basically, paleoclimates follow the same kinds of regimens that the modern climates are following: where the oceans are, where the equator is, where the mountain ranges are, and so forth.

That means you can make broad predictions about what a paleoclimate would have been based on its relationship to the equator or based on the presence or absence of nearby mountains. I use these kinds of principles to show more arid areas versus more humid areas.

The next three sequences show the evolution of the Earth's surface in reverse, from the present day to, at the very bottom, 600 million years ago, when nearly all of the planet's landmasses were joined together in the Antarctic. The first sequence shows roughly 90 million years of backward evolution, the continents pulling apart from one another and beginning a slow drift south. They were mapped using the Mollweide projection, and, in all cases, are by Ron Blakey.



Twilley: And you paint the arid area based on a contemporary analog?

Blakey: Right. I know the modern world reasonably well and I’ll choose something today that might have matched the texture and aridity of that older landscape.

I use a program called GeoMapApp that gives me digital elevation maps for anywhere in the world. Most recently, they have coupled it with what they call the “Blue Marble.” NASA has stitched together a bunch of satellite photos of the world in such a way that you can’t tell where one series of photos come in or another. It’s a fairly true-color representation of what Earth would look like from space. So this Blue Marble is coupled with the GeoMapApp’s digital elevation topography; you put the Blue Marble over it, and you use a little slider to let the topography show through, and it gives you a fairly realistic looking picture of what you’re looking for.

For example, if I’m working with a mountain range in the southern Appalachians for a Devonian map—well, the southern Appalachians, during the Devonian, were probably far enough away from the equator that it was in the arid belt. There are some indications of that, as well—salt deposits in the Michigan Basin and in parts of New York and so forth. Plus, there are red-colored sediments, which don’t prove but tend to indicate arid environments. This combination tells me that this part of the world was fairly arid. So I’m going to places like modern Afghanistan, extreme western China, northern Turkey, or other places where there are somewhat arid climates with mountain belts today. Then I clone the mountains from there and put them in the map.

But you have to know the geologic background. You have to know how the mountains were formed, what the grain of the mountains was. That’s not always easy, although there are ways of doing it. To know the grain of the mountains, you need to know where the hinterland and the center of the mountains were. You need to know where the foreland area is, so that you can show the different styles of mountains. You have to move from foreland areas—which tends to be a series of parallel ridges, usually much lower than the hinterlands—to the center and beyond.

I use this kind of information to pick the right kind of modern mountain to put back in the Devonian, based on what that Devonian landscape probably had a good chance of looking like. Do we know for certain? Of course not. We weren’t around in the Devonian. But we have a good rock record and we have a lot of information; so we use that information and, then, voilà.

To give another example, let’s look at the Devonian period of the east coast. The big European continent that we call Baltica collided with Greenland and a series of micro-continents collided further south, all the way down at least as far as New Jersey, if not down as far the Carolinas. We know that there are places on Earth today where these same kinds of collisions are taking place—in the Alps and Mediterranean region, and the Caucasus region, and so forth.

We can use the concept that, if two plates are colliding today to produce the Caucasus mountains, and if we look at the style of mountains that the Caucasus are, then it’s reasonable to think that, where Greenland and Baltica collided in the Silurian and the Devonian, the mountains would have had a similar style. So we can map that.

This second sequence shows the continents drifting apart, in reverse, from 105 million years ago to 240 million years ago. They were mapped using the Mollweide projection, and, in all cases, are by Ron Blakey.



Manaugh: That collision alone—Baltica and Greenland—sounds like something that would be extremely difficult to map.

Blakey: Absolutely. And it’s not a one-to-one relationship. You have to look at the whole pattern of how the plates collided, how big the plates were, and so forth.

Then there’s the question of the different histories of particular plates. So, for example, most of Scotland started out as North America. Then, when all the continents collided to form Pangaea, the first collisions took place in the Silurian-Devonian and the final collisions took place in the Pennsylvanian-Permian. By, say, 250 million years ago, most of the continents were together. Then, when they started to split apart in the Triassic and Jurassic—especially in the Triassic and Cretaceous—the split occurred in such a way that what had been part of North America was actually captured, if you will, by Europe and taken over to become the British Isles.

Scotland and at least the northern half of Ireland were captured and began to drift with Europe. On the other hand, North America picked up Florida—which used to be part of Gondwana—and so forth.

One of the things that is interesting is the way that, when mountains come together and then finally break up, they usually don’t break up the same way that they came together. Sometimes they do, but it has to do with weaknesses, stress patterns, and things like this. Obviously, all time is extremely relative, but mountains don’t last that long. A given mountain range that’s been formed by a simple collision—not that there’s any such thing as a simple collision—once that collision is over with, 40 or 50 million years after that event, there is only low-lying landscape. It may have even have split apart already into a new ocean basin.

But here’s the important part: the structure that was created by that collision is still there, even though the mountains have been worn down. It’s like when you cut a piece of wood: the grain is still inherited from when that tree grew. The pattern of the grain still shows where the branches were, and the direction of the tree’s growth in response to wind and sun and its neighbors. You can’t reconstruct the tree exactly from its grain, but, if you’re an expert with wood, you should be able to look and say: here are the tree rings, and here’s a year where the tree grew fast, here’s a year where the tree grew slow, here’s where the tree grew branches, etc.

In a sense, as geologists, we’re doing the same things with rock structure. We can tell by the pattern of how the rocks are deformed which direction the forces came from. With mountains, you can tell the angle at which the plates collided. It’s usually very oblique. What that tends to do is complicate the geologic structure, because you not only get things moving one way, but you get things dragging the other way, as well. But we can usually tell the angle at which the plates hit.

Then, in many cases, based upon the nature of how the crust has been deformed and stacked up, we can tell the severity of the mountain range. It doesn’t necessarily mean that we can say: oh, this structure would have been a twenty-thousand-foot high mountain range. It’s not that simple at all, not least of which because rocks can deform pretty severely without making towering mountains.

This final of the three global sequences shows the continents drifting apart, in reverse, from 260 million years ago to 600 million years ago. There was still nearly 4 billion years of tectonic evolution prior to where these maps begin. They were mapped using the Mollweide projection, and, in all cases, are by Ron Blakey.



Manaugh: Are you able to project these same tectonic movements and geological processes into the future and show what the earth might look like in, say, 250 million years?

Blakey: I’ve had a number of people ask me about that, so I did make some global maps. I think I made six of them at about 50-million-year intervals. For the fifteen to 100-million-year range, I think you can say they are fairly realistic. But, once you get much past 75 to 100 million years, it starts to get really, really speculative. The plates do strange things. I’ll give you just a couple of quick examples.

The Atlantic Ocean opened in the beginning of the Jurassic. The actual opening probably started off the coasts of roughly what is now Connecticut down to the Carolinas. That’s where the first opening started. So the central part of the Atlantic was the first part to open up. It opened up reasonably simply—but, again, I’m using the word simple with caution here.

The north Atlantic, meanwhile, didn’t open up until about 60 to 50 million years ago. When it opened up, it did a bunch of strange things. The first opening took place between Britain and an offshore bank that’s mostly submerged, called Rockall. Rockall is out in the Atlantic Ocean, northwest of Ireland—near Iceland—but it’s continental crust. That splitting process went on for, let’s say, ten million years or so—I’m just going to talk in broad terms—as the ocean started opening up.

Then the whole thing jumped. A second opening began over between Greenland and North America, as Greenland and North America began to separate off. That lasted for a good 40 or 50 million years. That’s where you now get the Labrador Sea; that is actual ocean crust. So that was the Atlantic Ocean for thirty or forty million years—but then it jumped again, this time over between Greenland and what is now the west coast of Europe. It started opening up over there, before it jumped yet again. There’s an island in the middle of the North Atlantic, way the heck up there, called Jan Mayen. At one time, it was actually part of Greenland. The Atlantic opened between it and Greenland and then shifted to the other side and made its final opening.

The following two sequences show the evolution of Europe from an Antarctic archipelago to a tropical island chain to the present day Europe we know and recognize. The first sequence starts roughly 450 million years ago and continues to the Jurassic, 200 million years ago. All maps by Ron Blakey.



So it’s very complicated. And that’s just the Atlantic Ocean.

The Northern Atlantic took at least five different paths before the final path was established, and it’s all still changing. In fact, the south Atlantic is actually even worse; it’s an even bigger mess. You’ve got multiple openings between southwest Africa and Argentina, plus Antarctica was up in there before it pulled away to the south.

These complications are what makes this stuff so interesting. If we look at events that we can understand pretty well over the last, let’s say, 150 or 200 million years of time—where we have a good indication of where the oceans were because we still have ocean crusts of that age—then we can extrapolate from that back to past times when oceans were created and destroyed. We can follow the rules that are going on today to see all of the oddities and the exceptions and so forth.

These are the kinds of things I try to keep track of when I’m making these maps. I’m always asking: what do we know? Was it a simple pull-apart process? There are examples where continents started to split across from one another, then came back together, then re-split in a different spot later on. That’s not just speculation—there is geologic evidence for this in the rock record.

So, when it comes to extrapolating future geologies, things become very complicated very quickly. If you start thinking about the behavior of the north Atlantic, creating a projection based on what’s going on today seems, at first, like a fairly simple chore. North America is going on a northwesterly path at only one or two centimeters a year. Europe is moving away, at almost a right angle, at about another centimeter a year. So the Atlantic is only opening at three centimeters a year; it’s one of the slowest-opening oceans right now.

OK, fine—but what else is happening? The Caribbean is pushing up into the Atlantic and, off South America, there is the Scotia Arc. Both of those are growing. They’ve also identified what looks like a new island arc off the western Mediterranean region; that eventually would start to close the Atlantic in that area. Now you start to speculate: well, these arcs will start to grow, and they’ll start to eat into the oceans, and subduct the crusts, and so forth.

Again, for the first 50, 75, or even 100 million years, you can say that these particular movements are fairly likely. But, once you get past that, you can still use geologic principles, but you’re just speculating as to which way the continents are going to go.

For instance, the one continent that does not seem to be moving at all right now, relative to anything else, is Antarctica. It seems to be really fixed on the South Pole. That’s why some people think that everything will actually coagulate back towards the South Pole. However, there are also a bunch of subduction zones today along southern Asia, and those are pretty strong subduction zones. Those are the ones that created the big tsunami, and all the earthquakes off of Indonesia and so forth. Eventually, those could pull either parts of Antarctica or all of Antarctica up toward them.

But I’m more interested in reconstructing the past than I am the future, so I’ve only played around with those five or six maps.

This second sequence, showing the next phase in the evolution of Europe, begins approximately 150 million years ago and extends to the present day. All maps by Ron Blakey.



Manaugh: To ground things a bit, we’re having this conversation in Flagstaff, on the Colorado Plateau, which seems like a great place to teach geology. I wonder whether there might be another Colorado Plateau, so to speak, elsewhere in the world—something geologically similar to the extraordinary landscapes we see here that just hasn’t had the chance to emerge. Maybe the tectonics aren’t right, and it’s still just a crack, rather than a canyon, or maybe it’s covered in vegetation or ice so we can’t see it yet. Conversely, I’m curious if you might have found evidence of other great geological districts in the earth’s past—lost Grand Canyons, other Arches National Parks—that have been lost to time. How could we detect those, and where are they?

Blakey: This is indeed a great place to teach geology. It’s a great place to live.

As for Colorado Plateau analogs—it’s an interesting question. There’s an area in South America that I’d say is fairly similar. It’s got a couple of famous national parks that I can't remember the name of. It’s a smaller version, but it’s very similar to the Colorado Plateau. It’s between the Andes and the Amazon basin, part of the general pampas region there of South America. It even has similarly aged rocks. Parts of northern Africa would also be similar.

But you have to look at all the characteristics of the Plateau. Number one: the rocks are flat. Number two: the rocks have been uplifted. Number three: the rocks are dissected by a major river system. Number four: it’s a semi-arid climate. There are probably five or six defining characteristics in total, and I’ve heard many people say that there is no other place else on Earth that has all those characteristics in exactly the same way. But I went to an area in eastern Mauritania many years ago, where, for all the world, it looked like the Grand Canyon. It wasn’t as colorful, but it was a big, deep canyon.

In fact, the Appalachian Plateau would be somewhat similar, except it’s in a humid climate, which means the land has been shaped and formed differently. But the Appalachian plateau has flat-lying rocks; it’s dissected by some major rivers; it’s experienced uplift; and so forth.

The next two sequences of images, followed from left to right, top to bottom, illustrate the gradual evolution of the Colorado Plateau, where, in its modern day incarnation, this interview with Ron Blakey took place (specifically, in Flagstaff, Arizona. The earliest map included here depicts the Proterozoic; the first sequence ends in the Triassic. All maps by Ron Blakey.



Twilley: I’m interested in the representational challenges you face when you decide to make a map, and, specifically, when you’re in Photoshop, what your most-used tools might be. I thought it was fascinating when you said that the cloning tool really changed how you make geological maps. What other techniques are important to you, in order to represent geological histories?

Blakey: Oh, the cloning tool is the most important, by far—at least when I’m actually painting. Of course, I use the outline tool to select areas, but, when I’m actually painting, it would be impossible to paint these different maps pixel by pixel. I couldn’t do it. Occasionally, I will actually hand-draw some things in the flatlands, where I want to put a river system, for example, but, at least for mountains and rugged terrain, I clone everything.

Some times, I’ll cut and paste. I’ll select an area in the GeoMapApp, I save it as a JPEG, and then I can select it and copy it and paste it in, and I can rotate and deform it a little bit. Are you familiar with the warp tool in Photoshop? I use that a lot, because you can change the shape of mountains a little. If you do it too dramatically, it really looks flaky. But, if you do it right, it still looks pretty realistic.

This second sequence, also showing the evolution of the Colorado Plateau, begins with the Triassic and ends roughly 5 million years ago—basically the present day, in geological terms. All maps by Ron Blakey.



Twilley: And do you have certain filters you rely on for particular geological effects?

Blakey: A little bit. I like to use the craquelure filter. It actually gives you little bumps and valleys and so forth. I use that especially for continental margins. Continental margins are anything but regular slopes, going down to the abyssal depths. They’re very irregular. There are landslides and all kinds of things going on there at the margins, so I add a little texture with craquelure.

It can be difficult to use, though, and it doesn’t work at really high resolutions—so, what I actually have to do some times, is that I will actually copy a part of my map, take it out, make it smaller, do the craquelure on it, and then blow it back up and paste it in again.

A painting by Ron Blakey depicts a geological landscape near Sedona, Arizona.

Dee Blakey, Ron's Wife: I think the other reason that he can do what he does is that he paints. That’s one of his paintings, that one over there [gestures above fireplace].

Blakey: Well, I guess I should have said that right away, when you asked me why I got interested in this, because I am interested in the artistic aspect of geology. The artistic aspect of science, in general, but especially geology. Astronomy, for example, would be another field where artistic visualizations are useful—any time you’re trying to show things that can’t easily be visualized with something comparable here on present-day planet Earth, you have to use an artistic interpretation.

Anyway, I can’t explain it, but I understand color pretty well. I use the hue saturation tool a lot. I’ll select an area and then I’ll feather it, let’s say, because you don’t want the edges to be sharp. I’ll feather it by thirty, forty, fifty pixels. Then I'll take the slider for hue saturation, where, if you go to the left, you make things redder and, if you go to the right, you make things greener. If I’ve got a landscape that looks a little too humid, I’ll just slide it slightly to the left to make it a bit redder. You can also change the lightness and darkness when you do that. There’s also regular saturation. By killing the saturation, you can really kill the nature of a landscape quite a bit.

And I use hue saturation a lot. That took me a long time to master, because it’s really easy to screw things up with that tool. You start sliding things a little too far and, whoa—wait a minute! All of a sudden, you’ve got purple mountains.


On a hot afternoon in Moab, Utah, Venue stopped by the museum collection storage facility for the Southeast Utah Group of National Parks, to visit a small collection of objects and historical artifacts found within or associated with what are now Canyonlands and Arches National Parks.

We spent several hours in the company of curator Vicki Webster, who generously, patiently, and enthusiastically showed us through the collection, from 20th-century Park maps to ancient stone knives, from the eye-popping "bat drawer" and exquisite herbaria to corncob sandals, dinosaur bones, and pieces of pottery collected from the sites of southeast Utah's extraordinary National Parks.



Having just spent the previous week exploring these sites on our own, hiking various trails, visiting Newspaper Rock, and seeing as many of southern Utah's parks as we could, we were already intensely curious about what it takes to administer the natural landscape and the interpretive infrastructure of a National Park, seen from the perspective of collecting, cataloging, and preserving the outdoors.

How are these practices changing over time, we wondered, and what should a collection of artifacts from the nation's most historically and naturally significant landscapes include? How are these objects narratively explained and physically maintained for future generations? Further, how do even the trails themselves function as a kind of museum without walls—and what goes into designing and documenting them?

Finally, how might archival practices oriented toward immersive experiences of outdoor landscapes differ from, for instance, the organizational techniques of a librarian, as Venue explored in our behind-the-scenes tour of the Denver Public Library with Wendel Cox?



Webster—a dream guide to this material, as curious about and excited by the collections as we were—told us countless stories of the region's parks. Many of these tales appear below, in the following edited transcript of our day spent behind the scenes of our nation's outdoor heritage, including the surprise natural gas pipeline that runs through Arches National Park and the possible future history of Blue John Canyon where hiker Aron Ralson infamously became trapped for 127 hours.

We were joined by a student named Malia, who was shadowing Vicki Webster for the day in order to learn more about the National Park Service.

• • •

Geoff Manaugh: Could you tell us briefly about the room we’re now standing in? At first glance, it seems to be more of an office archive or a storeroom, rather than a museum.

Vicki Webster: And it’s a very full storeroom! [laughs] You can see behind you that these shelves are just full of historic photos—so are these [gestures at shelves]—and they have all now been catalogued. We’ve also got three archival racks that are just about full now. These mobile racks are also almost full. I have a little space left in here, but not much.

The herbarium cabinets are right here, as well; then these specimen cabinets are where most of the archaeological and historical objects are. The archives are in these racks, and some other racks in the room on the other side of that wall. Then we also have map cabinets for oversized documents, drawings, and maps. We’re getting to where it’s pretty close-quarters.

In addition, we have some archival collections stored at the Western Archaeological Center in Tucson and at the Heritage Center in Dolores. We do have a lot—but, twenty years ago, there was really nothing catalogued, in terms of archives.



Nicola Twilley: In terms of the broad categories of collections that are stored here, I guess there would be natural history…

Webster: That’s exactly what I was going to start with, to give you an idea of the different disciplines. I pulled out some samples from each. If you look just behind you here, on this shelf, this is a single sauropod vertebra. When I show this to people I always say: take one hand and put it on your own spinal column, and feel the size of a single vertebra. Now look at this again—this thing is huge. And there’s another one there, and then there are some smaller ones.

A lot of people get really excited about archaeological things that are 800 to 1,200 years old—but these are millions of years old. This is a sign of life millions of years ago. To me, that’s much more fascinating and cool.

We do have these kind of paleontological resources in the collection, all found within the park boundaries. They were brought in from the field precisely because we didn’t want them to be stolen or damaged out there. In fact, we just recently finished a paleontological survey of Arches National Park, so the Utah state geologists have gone out there to a number of sites.



Twilley: Is that the oldest thing in the collection?

Webster: I would definitely say that our paleontological resources are among the oldest things in the collection. As to which one’s the oldest? Is it this particular vertebra? I don’t know. I’d have to look at these with someone.

But that’s really a large part of what I do: managing data. That data management function is critical, even more than having personal familiarity with the collection, so that other people can access the collection as a resource.

A lot of people associate the word curator with a subject-matter specialist, and, certainly, in a lot of museum work, you would have a subject-matter specialist as the curator. But, really, much of the time in National Park Service areas, the museum curator is a manager of the objects and the archives and the data about those objects, much more than a subject-matter specialist.

In some of the historic areas, a place like Gettysburg or the Civil War parks or Independence Hall, you’re more likely to have a historian dealing with the collections. But, in your big national parks, you’re going to have somebody who’s more of a manager than a specialist.

Also, I should say my background is in biology. Everyone thinks that if you’re the curator, you must be an archaeologist, but no—I’m not an archaeologist. I always like to make that little disclaimer, because, otherwise, I get asked a lot of questions where I have to say, “I don’t know, ask the archaeologist!”

Now, back to our discussion of different disciplines. We do have geologic specimens, as well, but not really here in our storage area. Geologists who come to the park to do research will generally take their specimens back to their respective institutions with them. What I do, in that case, is administer loan agreements with them; we retain that documentation and they retain the specimens.



Twilley: Is that a common occurrence? In other words, are there a lot of rock samples out there that came from Canyonlands and Arches, but are now distributed around the country or even the world?

Webster: Well, a lot is a relative term. In terms of Canyonlands, there’s consistent interest in places like Upheaval Dome—a geological formation that’s fairly mysterious. There’s been some speculation that it was formed as a salt uprising, as well as some speculation that it’s the result of a meteorite impact. A lot of geologists have come here over the years to study that specific controversy. This year, we even have some geologists looking at the possibility that it’s the result of a combination of both of those factors—that perhaps it was both a meteorite impact and a salt upheaval—and they’re trying to look at whether that could be the case, and what the sequence of events might have been.

[points at map] There—that’s the Upheaval Dome. You can see, to a geologist, that this would just jump out at you. You’d say, “Hey, this is something strange and weird. What is this? We don’t normally see circular formations like that.” That’s something for which we write research permits almost every year, and some long-term studies have also been done on it.

Twilley: When they take the rocks and you put together a loan agreement for them, do they actually show up with a truck full of rocks that you have to sort through for each loan agreement or can they just take the rocks and go? Do you actually see what they take?

Webster: Well, collecting rocks is illegal unless made by permit—and the permits severely restrict the quantity of material to be collected. It can only be a very small amount.

In terms of your question, I don’t always see it, because they don’t always physically come into the office and bring the samples here, but it is documented and it is catalogued. Each sample is assigned a unique catalog number in our system, and they send me the data. I can then say that you have rock number so-and-so, and here’s how big it is and here’s what it looks like and here’s all the data about it. Because I’m not a geologist, I don’t always understand all the technical data, but I always insist they give it to me for our records.



Twilley: So there’s an inventory here of rocks that have been moved elsewhere.

Webster: Yes. If I want a list of all the geologic specimens that have been collected from Canyonlands and are on loan elsewhere, I can spit that out from my database. Absolutely. Once in a while, the samples will even come back to us—somebody will retire or whatever, and their collection will be returned.

For example, there’s a box right there that’s full of rocks. [turns to box on shelf] These are geologic specimens that were collected from Upheaval Dome. These are called shatter cones and they were collected by one of the researchers who had been finding evidence of meteorite impact. You can see that these are labeled; they have numbers on them. To a geologist, this looks very different from other rocks. In fact, even to a layperson it looks like there’s some impact evidence.

While we’re talking about natural resources, back in the day—this is back in the 1940s, 50s, and 60s—we used to slaughter park wildlife in order to study it. That means that we have a number of bird and rodent specimens and things like that in the collection, as well. We don’t do that so much anymore, as there are many other—and better—ways of studying wildlife without killing it.

But I do like to pull out the bat drawer to show it to people, because the bats are really fascinating to me. [pulls out the bat drawer]

Manaugh: Oh my god.



Webster: We have a variety of bat species in the park. When you’re out camping, and it’s evening, and the bugs are out, the bats start to fly around and catch things, but they all kind of look the same to me as they fly by. I think, “Oh—bat.” But they’re really very different.

We have big-eared bats, Mexican free-tailed bats, little bitty pipistrelles—there have been some pretty thorough bat surveys done here, too. We had an interpreter here years ago who did a great campfire program on bats. She was amazing. She’s one of these really creative, artistic interpreters. She would take a black, plastic garbage bag and get a visitor to stand up in front of everybody at the campground amphitheater, and she would attach the garbage bag to their little fingers and pull it all the way down to their waist, and then she would have the person demonstrate how a bat catches mosquitoes by scooping around and bending over and picking them up and eating them—because they trap the bugs in their wings. That’s what they do. It’s very cool.



We also have an herbarium for each of the four parks. In fact, I don’t know if I explained that there are four National Park Service sites that are served out of this office? This office is called the Southeast Utah group of parks, so we have Arches and Canyonlands National Parks, as well as Hovenweep and Natural Bridges National Monuments. Hovenweep and Bridges are to the south of us.

Manaugh: We just went through Bridges yesterday, actually.

Webster: Oh, isn’t it wonderful? What a gem. I just love that spot.

So we do have an herbarium for each of the four parks. And, although we do not have a voucher specimen for every known species—these are called voucher specimens [gestures at cabinets]—we do have a lot, and we’re working on completing the herbarium collection. When our staff is out in the field, they know which species are suspected to grow here and, if they should find one of those, they will collect a voucher specimen.

I don’t know how familiar you are with herbarium collections, but I pulled out a sample for you. A lot of people don’t realize that an herbarium collection is actually useful for a lot of things other than just the identification of plant species. Things like blooming dates can be very important. A few years ago, for instance, I was lucky enough to go to the Smithsonian for a curatorial workshop, and one of the things we got to do was play—it was work, of course, but for me it was play—in the herbarium at the Smithsonian. It was so much fun. For an old botany major like myself, I thought I had died and gone to heaven!

They showed us a study that had demonstrated how blooming dates are now about three weeks earlier than they were, I think, fifty years ago, or whatever specific date they’d been using. They have specimens from year after year over the decades, and the blooming dates are getting earlier because of climate change. So the herbarium specimens are going to be the evidence, another fifty years from now, for how species began migrating in elevation because of climate change. There’s actually a lot of information in an herbarium collection.



Twilley: Are you responsible for mounting them and putting together the display?

Webster: Some of the time. It depends.

We had an ecologist here for a number of years who would press his own specimens and then hand them over to me, newspaper and all, and I would mount all his stuff and label it. Right now we have a person working here who is really good at doing beautiful mounting. She loves to do it. She delivers these gorgeous specimens to me, all ready to go. All I have to do is enter the data.

When I do it, I actually work from a reference book about herbarium specimens, including how to handle them and how to mount them, even how to create a little envelope for the seeds or cones. A lot of it is about making sure what’s visible are the critical parts for identification purposes. Of course, that starts at the moment of collection and at the moment of pressing, but also at mounting time. Some specimens are more challenging than others. Cacti are particularly challenging, as are really long grasses because of their size.

Manaugh: You mentioned that the herbariums would be finished at a certain point. What’s the actual finish line, and how do you judge completion?

Webster: Well, I used the word complete, but I meant complete in the sense of species representation. We have a list. In fact, one of the things I have to do as collections manager is to write a “Scope of Collections” statement that says what is appropriate for us to accession into the collection. That statement includes an appendix that lists all the various plant species that are believed to grow in the park, but for which we don’t yet have a voucher specimen. So, presumably—I don’t know if I’ll live long enough—but, presumably, the day will come when that list will pretty much be checked off.

Twilley: Would you include invasive species on that list, as well?

Webster: Oh, absolutely. We have a large invasive species program here. We actually have an active set of employees whose job is to locate, identify, and get rid of invasive species.



Manaugh: This touches on the border between natural history and cultural history, but I’m curious where things like indigenous but cultivated plants would fit into this. In other words, how do you catalog a plant that is actually an agricultural remnant from an earlier culture, but that now appears to be “natural” to the region?

Webster: That’s a good question. In the mid 70s, there was a group of people from San Jose State University who did a huge research project at Hovenweep. It used to be that the Mesa Verde staff managed Hovenweep, but there was an administrative change and now it’s ours; so we’ve been receiving the Hovenweep collection here in fits and starts over the years.

As it started to trickle in, I was amazed that the herbarium seemed to be collected by the same guy at the same time in the mid 70s, and at first I thought this was really strange. Then, finally, I got enough information about their cultural collections to realize that this massive study done by San Jose State was actually about agriculture, which is why there were so many plant species.

So, yes, in the Hovenweep collection there are such things, definitely. At Canyonlands, there’s a spot where we found gourds that we think were being cultivated, so we have some specimens from there. But the intersection of natural and cultural resources is a fascinating topic.



Every once in a while I think I’ve got to write a book! I’ve got to make notes on all the collections here, because, yes, it’s very interesting.

You know, that’s another thing. Last spring, I hit a landmark birthday and became eligible to retire, so I’m starting to think about the fact that I’m not going to be here forever. This has a lot of repercussions. I’ve had this job for 20 years and, when I walk out the door, a lot of institutional memory is going to go with me. My biggest goal is to make that moment unimportant, from the perspective of the collection—to make it so, when I walk out the door, everything is documented and there are people here who know how to access the documentation, where to find it, and to ensure that it’s not all lost.

Manaugh: Back in the 90s, I interned at the American Folklife Center at the Library of Congress in D.C. It was right at the end of Joe Hickerson’s tenure there; he had been there, I think, since the archive’s founding several decades earlier, and he knew absolutely everything about the place. He knew the contents of random boxes, and even where, on specific audio recordings, you could find specific snippets of old songs—all these things about the collection that were unique to his own memory and experience of the place, including things that really weren’t written down anywhere. But you could tell that some of the staff were in a state of low-grade anxiety as they prepared for his retirement. The institutional memory that goes with that—that goes with just one person’s retirement—can be hard to duplicate.

Webster: It’s true. And, unfortunately, that’s where this place is going to be some time in the next two to three years. I haven’t decided when yet. But, you know, it’s a good feeling to be eligible to retire before you’re ready. Some people have the unfortunate experience of being ready long before they’re eligible—and I’m so thankful not to be there!



Anyway, I also pulled out a drawer from our entomology collection. I pulled this one out because these are underwing moths from Arches and Canyonlands. The entomologist who did this study actually discovered a subspecies of underwing moth that lives only in Arches; as far as we know, he hasn’t found it anywhere else. So, this is an example of a fairly recent study, done in the last decade, under permit in one of the parks, that resulted in new scientific findings and specimens.

Let’s move onto the cultural things. Malia actually asked me earlier if we have any cowboy stuff, because one of the parts of the cultural history around here is from the cattle ranching and grazing era—and, of course, grazing occurred inside Arches and Canyonlands National Parks until the 1970s. That’s not all that long ago.



Manaugh: It’s actually incredible how young some of the parks out here are.

Webster: Especially Canyonlands. We’re still a year and a half away from the fiftieth anniversary. Bridges, though, just had their 100th anniversary in 2008, and Zion just had theirs. In fact, because there were so many parks established around the time of the antiquities act, we’re starting to have a little rash of centennials. Rocky Mountain has got their centennial coming up, I think, and Crater Lake had theirs in ’02.

In any case, when Canyonlands was established—September 12, 1964, is the official date—there were active ranching operations going on and the grazing was phased out over time. That means there were still cowboy camps, because, when the cowboys left, they didn’t take everything with them. They just left it there. Actually, these things here came out of the Cave Spring cowboy camps—so if you were to go down to the Needles, you can actually drive over, park, and walk about one hundred yards over to the cowboy camp, and, even today, there’s still a lot of horse tack and empty coffee cans and stuff like that. There are tables and chairs, and an old stove. This [pointing at object in collection] is just a little bowl that was in the cowboy camp.



Twilley: And how is it that you have this bowl here, but there are still coffee cans out in the field? Why did you collect one and not the other?

Webster: Good question. Back in the 70s or 80s, somebody decided that some of the objects there ought to be called museum property, so they accessioned them into the collection, and they catalogued them, but then they physically left them out there. So, I’ll confess, I used to use that as my excuse to go out in the park once a year to check on them, because I didn’t really join the park service to spend all day indoors. But, then, finally, we had a collections management plan written, and one of the issues it addressed was what exactly we should do with this stuff. After all, when it’s outdoors, we can’t provide appropriate climate control and the objects are vulnerable to theft.

We finally decided that the thing to do was deaccession things that we had documented, and that really could just stay out there in the park, because it’s a place that visitors go to learn about the cattle-ranching era. That means it has value as an interpretive display. For example, there are always a ton of baking powder cans at these places—they seemed to use a lot of baking powder. I think they made a lot of biscuits. Then, some of the objects that did seem a little more valuable, and a little more vulnerable, were brought in. I have a few glass bottles and this bowl.



Manaugh: When you deaccession an object, does that mean it just stays out in the field or do you actually take it out of the archive and return it to the outdoor setting?

Webster: It stays in the field. It was already out there; it had never come in; and, really, it was probably an error of judgment that it had been documented as a museum object at all. If you’re going to call it a museum object, then bring it in and store it properly—or don’t call it a museum object.

Twilley: Can you just document it, but not accession it?

Webster: That’s something our cultural resources people do, but then it’s not part of the museum. It’s documented as a cultural site. It’s monitored. They go out there and photograph it and make notes and make sure it’s not being impacted and so on and so forth. But that’s a whole different function than the museum collection.

Manaugh: I’m curious, if some of those cowboy camps from the 1960s are now considered historic, what’s the timeline for, say, somebody’s climbing equipment or a Nalgene bottle left behind by a hiker in 2010—when would something like that become eligible for accession as an historical object?

Webster: You mean, when does trash become historic? Fifty years.

Manaugh: Fifty years? Is that just a rule of thumb or is there a genuine policy?

Webster: I think it’s in the National Historic Preservation Act—but, yes, fifty years is the cutoff point after which something can be considered historic. I had a little identity crisis when I turned fifty. [laughter] I was like no, no, no. I’m historic.

Manaugh: This is sort of a goofy question, but it seems as though every person we’ve sat next to at a restaurant or coffeeshop around here for the last week has mentioned, at some point, the movie 127 Hours. That took place not far from Moab. As far as “sites” like that go—I mean the slot canyon where Aron Ralston was trapped, and that was documented in the film—is there any sense that a location like that, that people all over the world now know about, should be preserved or marked somehow? In fifty years, perhaps? It’s like the Donner Pass, in a sense—it’s a cultural site where an historic event occurred.



Webster: That’s a good question. [pauses] That canyon is actually right outside park boundaries—it’s not inside the park—so our staff wouldn’t actually be addressing that question. But let’s pretend it is inside park grounds: would it be managed as a cultural site? You know… Certainly, over time, it would become part of the park’s history. But would we mark it, or preserve it?

One of the things I do here is put documentation into the archives. The 2002 Olympics in Salt Lake City took place not very long after September 11, 2001. The Olympic torch made its debut in the state of Utah under Delicate Arch at dawn in February, where it was very, very, very cold, and the logistics and the planning and the security for that event were absolutely phenomenal because it was so soon after 9/11. So, while that was going on, I was very much in touch with the people who were organizing it, and I was constantly saying: “Remember, I’m going to want the documentation. When this is over, give me your files.” Now, I have a really great little collection about all the planning and the photographs of that day. Even though it was a current event, I knew it was going to become part of the park’s history.

When something’s happening, you need to grab the documentation now. If you let it sit around for ten years, it might just disappear. You know, “Oh well, the guy who did this has been transferred, and he took his files with him,” or “the guy who did that has retired, and he doesn’t remember anything.” That sort of thing happens all the time.

Now, in the case of Aron Ralston’s story, there were park rangers involved in it, because, when he was rescued, our staff was just about to go out and start looking for him. They had been mobilized as part of the search effort. That means that it would be the sort of incident that would show up in the documentation that rangers create, and that might eventually make its way into our archives—or not.

So it’s an interesting question. Would Blue John Canyon, where Ralston was trapped, become considered a cultural site…? Maybe not until a few more decades have gone by.

Ultimately, that’s the sort of decision that the cultural resources program manager makes. Actually, here’s an interesting thing: we’re working on trying to get the site out at Arches where Edward Abbey’s trailer was listed on the national register. You wouldn’t have done that in 1957, when he was living there, but certainly, now, it seems appropriate. It seems historic. By the same token, then, right now Aron Ralston getting himself in a bit of a pickle is an interesting news story—but, twenty years from now, will it be a culturally significant site? I think it’s about how things change over time.

In any case, Canyonlands is about to have its fiftieth anniversary, in September 2014, and I hope that will spur a fair amount of historical research and interest in the park.



Twilley: It was funny to hear you say that you used checking on those camp sites as an excuse to get out in the park. How often do you get a chance to get out in the park, and to what extent are you involved with things like trailside displays or other outdoor interpretive infrastructure?

Webster: I started my career in the Park Service as a park ranger/naturalist and as an interpreter. But, after a long story that I won’t tell, I ended up in curation—so I don’t get out in the field nearly as much as I would choose to, if I had a choice.

There are museum objects on display in several of our visitor centers. For instance, the Needles Visitor center, which is south of us, was built—and the exhibits all designed and installed—in the early 1990s. Maybe ’92 to ’94. When they did that, they did everything right. They had architects design a beautiful building in harmony with the landscape. It’s fabulous. They had our exhibit specialists scour the museum collections for appropriate objects to tell the story that they wanted to tell, and the visitor center incorporated those objects and stories into the exhibits. They had the specialists build mounts and everything. It’s just very well done. I manage those; to the extent that they need any attention, they are my responsibility.

Subsequently, in the twenty years I’ve been here, the Park Service has rebuilt every visitor center except for the little trailer that they use at the Maze. That’s the only one that hasn’t been rebuilt. Every time, they have said, “Oh, we don’t want museum objects on display, because then we have to do climate control and fire and security requirements, and we just don’t want to do that.” Then, every time they’ve finished the building, they’ve said, “Well, we would like that one thing…”

For instance, at Arches there is a meteorite on display that is a museum object. It’s the only museum object in that practically new visitor center. That visitor center is five years old, or six, at the most. It’s a really new facility, but it only has one museum object in it—and that’s a meteorite.

Now, the light levels and the climate control—all that stuff—is not up to museum standards. It is in a secure case, and we do monitor the temperature and the humidity, but the building wasn’t built to the specs that you would have for displaying museum objects today.

Twilley: Working with such a wide range of artifacts, of such different materials and ages, means the environmental conditions must be difficult to manage.

Webster: Right. It’s always a compromise. In this storage room, we try to keep it at 65 degrees and approximately 35 percent humidity—but we have metal objects that would be happier if it were drier, and we have paper objects that would be happier if it were right at 35 percent. But we have to compromise, because we have so many different materials. In a place that’s just archives or just ceramics, though, you can tailor things.

We do have a wide variety of really interesting archaeological materials. I thought I would show them to you in order of material type. Here, we have a lot of lithics—mostly projectile points and stone knives. I pulled out this knife, in particular, because it’s so beautiful. It’s an absolutely gorgeous piece of stone. When you look at these, you have to think: it can’t just have been utilitarian. They had to have been thinking about the aesthetics of the object, as well.



Twilley: Is that dated?

Webster: It could be. I’d have to look it up. But these two objects are dated simply in the sense that we know what type they are.

I actually know some archaeology here, and I’m going to show it off! These are both Clovis points. Clovis is the oldest-known culture in this region, at 10,000 to 12,000 years old. This one was found out in the Maze District of Canyonlands and this one at the Island in the Sky district.

The way you can tell a Clovis point from some other projectile point is through what’s called a fluke. At the base of the point, you can see an indentation; it almost looks like a thumb depression. That’s diagnostic of a Clovis point. If you’re outside, walking around, and you see one of these, call the nearest archaeologist. They will be very excited.

So these are actually very special, and the only thing from the Clovis culture that’s been found in this area. There could be other stuff; logically, there should be. If there’s anything, then there should be more. But who knows?



Twilley: Is that the kind of thing where people will go back to the site where it was found and mount a full-scale archaeological excavation?

Webster: I think, in both of these cases, that they had already assessed the area and found that these were just isolated finds that had been dropped. There was no real site associated with either one of those.

Now, we also have a number of vegetal objects—for instance, this is a fire stick, so you could drill and make a fire—and we have some sandals in our collection. One thing I’ve learned from the archaeologists is that this very tight, fine weave [showing us a pair of sandals] is older than the looser material. The looser, sloppier material seen in other sandals is actually more recent—and I figure this is a comment on the deterioration of civilization over time. Back in the day they had time to be very careful—and now we have flip-flops. [laughter]



Twilley: Are these shoelaces? [points at what appear to be threads visible on the outside of the sandals] These are pretty great shoes!

Webster: This is just some reed—and these are actually corncobs. Archaeologists will actually study the corncobs and count how many rows they have, because corn evolved and changed its form over time, so the number of rows, and the form of the corncob, can tell you something about the age of the corn.

Finally, I always pull this object out, because it’s fascinating. It’s made from a knucklebone, probably from a deer or a sheep, and it’s been carved into a Bighorn sheep effigy. If you look at it, you can see the hole; that had a string through it. Someone could have worn it, or hung it on something, or attached it to a ceramic object or stick. This was actually found near some rock art that showed Bighorn sheep, interestingly enough.



Ceramics, of course, are another thing we collect across the parks. This is an example of what’s called black and white Mesa Verdean. That would be the later Anasazi pottery, from the era of about 1100 to 1300. The painted pot—which is hiding back there on a shelf—could have been a kiva jar. It’s very fragile. There was probably a lip on it, like this one, and it was possibly found in a kiva. Actually, I’ll show you the shape of it; it’s quite lovely. The corrugated pots were used more for utilitarian things, like cooking. You know, I put it way back there, and now I can’t even reach it to pull it out where you can see it!

Twilley: Oh, I think I can see it. There’s a small soil sample next to it?

Webster: Yes, that would be what was found inside the pot. They pull things like that out and then they can check it for pollen, which can be dated.

Now, I pulled out this little pot so that I can tell you a story about it. This is a Hopi pot from about 1500. I have to look at it first; it always makes me nervous to pick it up. This pot was found with a couple of others—they’re similarly painted, from the same era and site—and those have been down in our conservation center being treated. One of them was full of salt. We have an archaeologist doing a study right now to source the salt and see where it came from, because we had thought that this was the farthest north that Hopi pots have been found. However, her research shows that, actually, there have been two or three sites even further north where Hopi pots have been discovered.

Well, the story of how we ended up with this pot is quite unusual. Back in the 1960s, there were a couple of families who worked at Arches National Park, who were out exploring in the area that we now call the Needles. They were taking a break somewhere, and they looked up and saw this big alcove with a rock slab across it. One of the women said, “You guys can rest, but I’m not that tired, and I’m going to run up there and take a look.” So she scrambles up there, looks behind this big slab of rock, and just starts screaming, “Pots! I found pots!”

There were two big, corrugated pots, three of these painted pots, and a bunch of gourds, along with some juniper bark and some shards—a big collection of stuff. It was just amazing to her. So they all went up there, and they looked at it, and they took pictures, but then they had to decide what they were going to do about it.

Of course, these were Park Service employees and, because of the Antiquities Act of 1908, they knew that they weren’t allowed to collect them. However, it’s the early 60s. The Glen Canyon Dam was being built, and Lake Powell was filling up; as it was filling, it drowned over 2,000 archaeological sites. There were archaeologists swarming all over the area trying to mitigate whatever they could before the lake came up and drowned those sites. There was even a widely believed but unfounded rumor that archaeologists had started breaking the pots they found so that they could ship them out easier and fit them into storage back at their universities.

Archaeologists exploring lands soon to be flooded by Lake Powell, summer 1958, courtesy of the Arizona Archaeological and Historical Society.

So you have to picture being these people, sitting up in this alcove with this amazing cache of stunningly beautiful Hopi pots, and believing in your heart of hearts that if you were to tell those “rotten archaeologists” about it, they would take a hammer to it all and just ship them off to a university store room somewhere. What would you do?

Well, they decided that the best thing for them to do was take the pots. Of course, the best thing to do actually would have been to leave them there—but they took them. They took photographs of the pots in place. They also had a map, and they marked where they had found them. And one of the people on the trip was keeping a diary, so she also described in detail the whole day and the whole event and everything that happened.

An unrelated shot of archaeologists documenting petroglyphs in Desolation Canyon, Utah, courtesy of the Colorado Plateau Archaeological Alliance.

Then they packed the pots out, and took them to their respective homes.

Twilley: They took them home?

Webster: They took them home. The woman who initially found the cache, of course, took most of the pots herself.

But, now, fast-forward about 40 years. Her husband has now passed away, she has remarried, to a lovely man; and they’re living in a suburb of Denver. The woman has taken ill, and she knows she’s not going to be around much longer, so she tells her husband: she says, “There’s one thing I want you to promise me. You’ve got to get those pots back to the park.”

So, out of the blue, unbeknownst to us—we had no clue that any of this had ever happened—the phone rings one day and it’s this gentleman. His wife had passed away, and he had something he would like to bring back to the park. He asked if he could deliver these pots she had taken. We said, “Oh, yeah, that would be fine.” We had no idea what they were.

So he wraps them up in some old quilts; he sticks them in the trunk of his car; and he drives all the way over from Denver. He shows up here in Moab, and he takes us out to the parking lot. He opens the trunk of his car—and there are these beautiful pots.

Twilley: Goodness me.

Webster: He very ceremoniously gave them back to the Park, including some of the documentation, which he had brought along with him, and that meant we knew who the other people had been, where they had found these pots, and that we could get in touch with them to find even more maps and photographs. These are actually very well documented—and now we’re able to study them.

So that’s a great little story of how something could have gone horribly wrong, but, eventually, if you wait long enough, decades later it can all come back.

Manaugh: How often does it happen that people feel guilty and actually return things that they’ve taken?

Webster: You know, almost never. But that example was unique—in fact, that whole story is quite unique. Of course, people do pick up flakes or cherts or rocks and stick them in their pockets. But then they go home and they have a car wreck or they break their leg or their house burns down—and occasionally they’ll send the stuff back, saying, “It must be bad juju—I’m sorry I took it.” Of course, what are we doing to do with it? We can’t put it back; we don’t know exactly where it came from. It’s just a sad story all around when people take things out of the park.

Now, sometimes we do use those returned objects for interpretive purposes, because the park interpreters can then say that, when you’re out in the field, if you find something like this, just leave it there. Please! If you really want to touch one, touch this one, which is one that has already, in effect, been ruined. But leave anything else in place. So returned objects do have an interpretive function, but it’s really not a scientific function anymore—because, once the context is gone, it’s gone. It’s been destroyed.

I have one more little story to tell you—and that’s about the object in these boxes. As you leave, and as you’re heading down the hall, look to your right and you’ll see an enormous poster that’s all about this next object I’m going to show you. You’ll see the pictures and you’ll say, “Oh, I just saw that!” and be very excited. This only happened about six or seven years ago.

Some visitors were over in the Horseshoe Canyon Unit of the park, where the Great Gallery rock art panel is. It’s a very famous rock art panel. There’s a sand dune at the base of it—and this object was just sticking out of the sand dune. It had eroded out. Fortunately, that day we had a ranger in the canyon. We don’t always have somebody in the right place at the right time, but that day we did. They were able to report it to the archaeologist, and it was brought in appropriately.



It’s a bag made from an antelope leg. See the stitching here? You can see that it was tied off to create separate little compartments. You can also see that there’s fresh rodent chew—in other words, tooth marks from rodents. That means it eroded out of the sand dune and, probably that same night, mice found it, thinking it was a free meal; and the next day, it was discovered by humans. Otherwise, the mice would have been back that night—and we’d never have found this object.

Twilley: That’s incredible.

Webster: What was in the portion that was chewed on by the mice is these little seeds. [we peer inside pouch] These seeds are marsh elder, one of those plants that we have not yet found inside park boundaries, but that we do know grows right outside park boundaries. So those seeds were all stuffed inside that softball-shaped portion of the bag.

Twilley: This whole thing is made from an antelope leg, you said?

Webster: Yes. We had an archaeologist from Flagstaff analyze this, and he determined that it’s an antelope leg. I don’t know how he determined that, but he did. [laughter] If you think about it, though, it makes sense: if you want to make a bag, you start with something that’s already close to the shape you’re looking for.



These three little bags were in this portion here. This stone was lying right on top. All three of these were just cram-packed into that compartment. And these two bags—this one and that one—were empty. This one, though, was very obviously full of something. As luck would have it, shortly after this came in, a woman from the University of Utah who is a specialist in fibers was here to look at our sandals and do some other work for us. So we said, “Gosh, while you’re here, would you open that bag for us?” Because nobody here is technically trained to do that sort of thing. So she was happy to play Indiana Jones for us. It was almost painful to watch her do this, but she very carefully sketched and photographed the knot before she ever touched it. Then she pulled one string—and she sketched and photographed the knot again. Then she pulled another string—and she made another sketch and took a photograph. Then another string… I mean, this went on interminably. We’re all standing there, just salivating. Is she ever going to open it? I don’t remember how long it took; I just remember we all thought it would never end.

Finally, she gets the bag open and we discover that inside are these forty-two little rock chips. Forty of them are a pink chert, which we know comes from an area just north of town—just north of the airport—called the Dubinky Well area. It’s a fairly unusual type of rock, so we sourced it to that location. But the other two were different—one’s brown and one’s clear—and we don’t really know where they came from. All forty-two of these little stone chips were cram-packed into this bag, as well as this little piece of antler.

The archaeologist who analyzed this describes it basically as a toolkit. You have your raw material—your flakes—and you’ve got the cobblestone here to use as a hard work surface. Using that, you could press your flake to make a projectile point, so that you could go catch dinner. If all that failed—if you didn’t catch dinner—here, you’ve got your handy dandy granola to survive on.



Twilley: Those seeds were their trail mix?

Webster: Basically. And this whole thing was their projectile point-making kit.

This object is unusual, partly because it’s so complete and partly because it tells the story of the activities of an individual. Normally, when archaeologists are out in the field studying sites, they’re looking at big-picture stuff: they’re looking at communities, at cultural groups, at community activities, at habitation sites, at entire ways of life. It’s rare that they find an object that tells the story of what one individual might have done. So it’s a fascinating little object.

That’s a kind of the top-of-the-pops smattering of representative objects that we have here in storage at the museum.



Manaugh: Before we leave the room, I have to ask, as something of a map obsessive: is there anything in particular in your map collection that might be cool to see before we go?

Webster: Let me think. The oldest maps we have are probably from the 1950s and 60s. Of course, we have more recently generated maps depicting boundary changes for the park. But, the best map? [pauses] If you’ll follow me—just help me rotate this rack out of the way, because it’s blocking access to the map cabinet—let’s see. Let me find my favorite map. We have a map that shows the original idea of what Canyonlands National Park should have been. We call it the Million-Acre Map. That’s much more acreage than what we actually set aside.

In fact, the story of the establishment of Canyonlands is pretty interesting. It was very controversial. I mean, it was the 1960s. What wasn’t controversial in the 60s, you know? [laughs] Oh, here it is. I knew it was close. The dotted line you see here is the hoped-for million acres.

The original idea for Canyonlands—Bates Wilson and Stewart Udall’s concept of what the park should be—is that it should preserve an entire ecosystem. It should be rim to rim for that ecosystem. But, because of the strong feelings of state and local people, including the fact that they wanted to retain lands available for mineral extraction and grazing, the park was reduced. It’s the same battle we fight today. Just how much do you set aside for recreation and preservation? How much do you set aside to be drilled and grazed? It’s the how much question.



Manaugh: While we’re on the subject, one thing that interests about this region is the relationship between the parks and the extraction industry. I’m curious about what sort of relationship you might have with companies involved in prospecting for uranium or other natural resources, and whether, or how often, they donate things they find to you at the Park Service.

Webster: To be honest, that type of prospecting or exploration doesn’t happen inside park boundaries. When it happens outside park boundaries, it’s viewed more as a potential threat—but your question is interesting, because it comes from a different premise—that extraction could be a benefit, that they could find things.

Right now, our experience is that if there’s oil or gas leasing on or near our boundaries, then there’s a concern about the viewshed and the impact on the park.

Malia: You also have to look at it from the point of view of what’s already been done to the park, and what’s going to continue being done to the park, as well. There are a lot of uranium trails that have gone through Canyonlands that you can’t see anymore, unless you know what to look for. White Mesa was a uranium trail, and now it’s used as the White Rim Trail. And there’s a pipeline that goes through Arches. We don’t tell visitors about it, but it is still maintained by the oil company. We let them come through.

Manaugh: Is it underground?

Webster: Parts of it are underground. Actually, the pipeline has an interesting history. It was built in 1955 and, if you were to look at a map of Arches in 1955, the park was shaped almost like an hourglass. There’s a big area, a skinny area, and a big area, and the pipeline crossed the skinny area. In 1955, they got permission to cross the park because it was only a mile or so across park property.



Of course, now the park has expanded, so it goes through quite a lot of the park. As they do with any gas pipeline, the company will fly over it and look for weaknesses, and, if they detect a weakness, they have to go in with heavy equipment and dig it up and repair it. There’s a huge amount of impact to the local resources. The vegetation is destroyed; there’s soil disturbance; you’re going to have tumbleweed coming in where, before, you didn’t. It has a big impact on the park.

Manaugh: Having read Cato Institute reports, for instance, about how we might privatize the National Park Service, there’s definitely an interest in—

Webster: I have a gut reaction to that. I’ve had conversations with people who honestly believe that a park that doesn’t take in enough money and entrance fees to keep itself operating should simply be closed. I fear that that’s a growing attitude, because of the whole philosophy that the market should drive everything. That’s a philosophy that’s becoming more and more prevalent in our culture, even when it comes to National Parks.

But it makes me nervous, because the parks will only exist as long as people allow them to exist. These are valuable parts of America’s natural and cultural heritage that we, as a society, have decided are worth protecting and saving whether they would survive in a commercial marketplace or not. In my personal opinion, privatizing the function of the NPS—making it profit-motivated, rather than preservation-motivated—could mean losing valuable parts of our heritage as Americans.



Manaugh: I just have one more question, if you don’t mind. I’m curious about the trail itself as a pedagogic experience. There’s the trail as an athletic experience—designed so that you can really get your heartrate up—as well as the trail as an aesthetic experience, featuring the best views and scenery, but then there’s the interpretive trail, where you visit a certain site for historical or even narrative reasons. That kind of trail is really a kind of outdoor museum. As a curator, does trail design, as a form of spatial data management, cross your radar at all—and is there a trail that you think would be particularly great for the park but that doesn’t yet exist?

Twilley: For example, it could be fascinating to have an alternative trail system that actually did take you past the pipeline. I feel that, often, trails are carefully curated to give you what seems like a natural experience, yet the story the trail is telling is inherently artificial.

Webster: That’s interesting—though I haven’t dealt very much with that sort of thing. When I think of trail design in these parks, I think of the trail to Delicate Arch. It’s a fabulous trail, because it was designed by a landscape architect in the 1940s, and I even have his file, which is how I know all this. When you hike up there, you don’t see your destination until you’re really there. It’s designed in such a way that you come around the bend—and, wham, Delicate Arch is right there, in your face, and it is just shockingly magnificent. You can’t prepare yourself for it, and I think he designed the trail that way. In fact, I know he did, because I’ve read his file. It’s very intentional. It’s a beautifully designed hiking experience.

But I know that, once in a while, an interpreter will do a program about the human side of National Parks: the maintenance side or recycling, as we’re really trying to green the parks and get people to recycle. We’ll have occasional programs—but we haven’t dedicated trail space to it. It would be interesting to think about how that might change the park.

Twilley: It might help make people aware that this is a choice we’ve made—that these parks are the way they are because we maintain them like this. They are something that we’ve built—not just something that exists, like putting a fence around a pretty part of nature.



Malia: If you ever go to the Windows section of the park, you’ll see the designated trail—but you’ll also see lots of different trails, running all over. Those are interesting.

Webster: That’s right—the social trails. But it’s pretty rare, now, that new official trails are built. Trail creation is something that tends to happen early on in the life of a park, and not as much as time goes forward. For the most part, people don’t seem to want to mess with the landscape after the park’s been established.



Twilley: Finally, you’ve worked at other parks, right?

Webster: Yeah. I’ve been here for 20 years but, before that, I worked in a bunch of other parks. I was recently travelling with some other old parkies and I was number two for number of parks worked at. I’ve worked at 15 parks total. I worked at the Everglades one winter, and at the Apostle Islands for about two and a half years. That’s in northern Wisconsin, on the shores of Lake Superior. But I’ve also worked at Yosemite, Saguaro, Colorado National

Manaugh: Where are you originally from?

Webster: Well, I’m half Texan and half Californian. I’m an old, fourth generation native-born Texan, but we left when I was 10 years old. I did most of my growing up in the Sacramento Valley, in Davis, California.

I worked in interpretation for a long time. I was the chief interpreter at Whiskeytown in the early 80s, which is also in northern California. Every park has collections that somebody has to take care of—but most of those people are not curators. A lot of the time, it falls on someone in the interpretive division. But I did a lot of museum work. When I was working at Apostle Islands, the park was only 10 years old; I established a museum program and hired people to start cataloguing the fishery, lighthouse, and brownstone quarrying materials. And the same thing at Whiskeytown: I was responsible for the collections there. I worked on the collections at Saguaro, and I did a little in Colorado, as well.

I’ve worked at a lot of parks!


While in Denver, Colorado, Venue had the pleasure of making a childhood fantasy come true: an all-day backstage pass to the city's public library, complete with a private introduction to room after room full of maps, books, paintings, photographs, architectural drawings, and other collections documenting the people, places, and events that shaped the settlement and growth of the western United States.

The Denver Public Library building, designed by Michael Graves & Associates.

From a meandering tour of the new Postmodern library building, designed by architect Michael Graves in the 1990s, to a covetous browse through the city's old fire-insurance maps produced by the Sanborn Map Company, via a quick mention of the Denver Police Intelligence Files and a thorough bibliography of reference materials related to Denver's saloon cats, it was an exhilarating day of flipping through card catalogs, stepping behind closed doors, following off-limits stairways up to archives not usually open to the public, and learning more not only about the history of Denver and the West, but also about library science, more generally, and about our guide for the day, Senior Special Collection Librarian Wendel Cox, more specifically.

Venue's vote for best card catalog entry ever—a Franz Feneon-worthy novel in two lines, filed under "Horses. Biography."—was brought to our attention by Wendel Cox.

There's no real way, however, without writing our own Ulysses of the Denver Public Library—describing every unexpected turn of conversation, every artifact, every cross-connected historical reference (rabies to quarantine to the library's medical collections) and every other thing seen, read, or pored over in nose-to-paper levels of detail during the day—to encapsulate all that took place during Wendel's enthusiastic introduction to the collections; so, instead, we'll just focus on a few particular highlights, cartographic in emphasis and origin.

Senior Special Collection Librarian Wendel Cox shows us a hand-drawn map of New Mexico and Utah.

First, the fire maps.



The Sanborn Map Company produced, between 1866 to 2007, some of the most extraordinary and historically useful maps of the urban United States available in any collection today.



Almost all major municipal libraries in the country maintain voluminous back-stocks of them, their heavy pages over time thickened past the point of bendability by endless glued layer after layer of property updates, infrastructural upgrades, new construction, and the entire re-routing of streets and whole neighborhoods at a time.



Peeling, partially unstuck, and warped into curling waves like oceans, the pages play host to a century or more of built structures, renovations, and replacements, keeping close tabs on what can be insured, for how much, and under what circumstances.



These Sanborn maps are as near-total a catalog of the city's development over time as can be cartographically imagined, with almost every square inch built up into thick scabs of structures upon structures, upon even more structures.

Every pasted edge conceals a preserved strata of earlier revisions and additions, all but daring us to pick at it (we resisted), tempting us to pull ever so slightly at the looser corners, to lift up the surface layer and reveal the other city—there is the city and then there is the city, as novelist China Miéville might describe it, the two, surreally, existing in the same place at the same time—that lies beneath today's Denver, with its competing but complimentary property lines, a city out of synch with itself as you peel away the layers of history.



Each page, as Wendel showed us, turning carefully through the old volumes, is like a plank of wood at this point, archaeologies of layers laminated into something almost more like furniture.

These are books as Kafka might imagine them: enormous, absurd, and so preposterously heavy with the details of local history as to be physically unmanageable. They are books that could wound the librarians who handle them, slipping discs and offsetting spines, causing even historians to second-guess turning their pages.



But this (exaggerated) sense of physical threat is, of course, echoed in the book's content: as we navigated Denver's neighborhoods, we developed a sense for the city as a place of fire risks and dangerous proximities, a city of escape-assisting back alleys counter-balanced by wood-framed meeting halls, its spaces rated for their performance during events of conflagration.

And, in the process, we saw the city as a series of surfaces built up over time, fractally expanding across the Front Range.



The second thing—of many things—worth mentioning was a decidedly less antique item from the collection: a map and pamphlet, produced by the U.S. Geological Survey and compiled by Glenn R. Scott between 1972 and 2004, called Historic Trail Maps in Eastern Colorado and Northeastern New Mexico (you can download the accompanying 45mb PDF here).



As the map's introduction, written by former USGS Director Charles G. Groat—who recently resigned from the University of Texas in a controversy over financial ties to the fracking industry—explains, many of the "historic trails that were the primary pathways used by pioneers to open the Western United States" have been forgotten or erased entirely.

These trails, he continues, "have names that remain familiar today—Santa Fe, Overland, Cherokee, Trappers, Republican Fork, and Smoky Hill Trails. Some of those historic trails have long-since vanished or are now only faintly visible on today’s landscape."

Scott's map and pamphlet are thus an act of preservation, the USGS explains, saving for future generations the wide range of "historic marks left on the land by Native Americans, trappers, prospectors, early road builders, and settlers from about the 1820s to about 1900."

Put another way, Scott made a map of lost roads.

A long slice of the Glenn R. Scott's USGS map, showing lost roads, trails, and camps to the south and east of Denver, Colorado.

As Groat writes in his introduction to Scott's work, the routes and place-names gathered on the map tell the human history and usage of the Coloradan landscape:

Features of the maps include trails used by Native American tribes and trappers before the arrival of European settlers. As the westward movement continued, trading posts, immigrant and prospector trails, stagecoach lines and stage stations, wagon roads, and railroads marked that expansion, and those features are shown on the maps. From the cattle trails and trails over mountain passes to the towns and military camps and forts, the settlement and use of these lands are captured for posterity. Routes taken by prospectors during the great 1859 Gold Rush to the Pikes Peak gold fields are portrayed, as are the world-famous mining camps that followed, including Central City, Blackhawk, Idaho Springs, Georgetown, Fairplay, Aspen, Breckenridge, Leadville, and Cripple Creek. In addition, the routes traversed by early explorers such as Zebulon M. Pike, Stephen H. Long, and John C. Fremont are shown on the maps. The maps reflect the Hispanic and French heritage of much of the region, and the rich history of New Spain, Mexico, and France are imprinted in the names of numerous mountain ranges, prominent peaks, valleys, rivers, and towns.

Scott's own story, meanwhile, is fascinating—equal parts folklore and geological survey of the American West:

Beginning in 1964, Scott realized that in addition to relating the geologic record there was an entirely different story he also wanted to tell. He was fascinated by the historic trails he encountered during his geology fieldwork—trails used by Native Americans and by pioneers and prospectors who settled in Colorado and New Mexico. He resolved to document those trails before they forever vanished. Using aerial photographs, long forgotten historical archives, and other historical texts, he located historic trails all over eastern Colorado and northern New Mexico, and in 1972 he published the first of his 11 historic trail maps.




Indeed, in a nicely circular reference, Scott himself writes that "most of the information I used came from the Denver Public Library, where I was a volunteer in the Genealogy and Western History Department." At the risk of over-using the analogy, he was a kind of James Joyce of the eastern Rockies, going back through deeds of sale, acts of incorporation for now defunct road-building companies, and, no doubt, Sanborn maps, in search of old ways across the landscape.

In a much longer pamphlet listing the sources used for his map, Scott gives some examples of the sorts of narrative coordinates that are all that remains of certain trails:

Starting at Bergen's house and down the gulch southeastward by the Hendershott's house to Myer's Mill on Bear Creek thence by the most practicable route by Luther's place and Parmalee's sawmill to the Turkey Creek Road at the mouth of the gulch opposite Parmalee's water mill on Turkey Creek.

Or:

From Boulder City, Boulder County, up and along north side of North Boulder Creek as far as practicable and best route to Central City, Gilpin County.

To which he occasionally adds his own surreal story-form updates, as if the information presented is now that much clearer:

Route was changed as follows: from American Avenue on the west bound- ary of Empire City extending 3 miles up the south bank of Clear Creek, then crossing and extending 3/4 mile up the north bank, recrossing and then 700 feet up the south bank, recrossing and then continuing up the north bank on the route designated in the original article, then up to and thru Vasquez Pass, then on the original route to Bangs or Corral Creek, the western terminus in the original article, then outside the area.

Perhaps most evocative of all, there are also entries that simply read:

Route unknown.



These are the "old ways," as author Robert Macfarlane describes the similarly forgotten trails and routes that spider the landscape of the United Kingdom. In his book of that name, Macfarlane writes that, "once you begin to notice them, you see that the landscape is still webbed with paths and footways—shadowing the modern-day road network, or meeting it at a slant or perpendicular. Pilgrim paths, green roads, drove roads, corpse roads, trods, leys, dykes, drongs, warns, snickets—say the names of paths out loud and at speed and they become a poem or rite—holloways, bostles, shutes, driftways, lichways, ridings, halterpaths, cartways, carneys, causeways, herepaths."

The incantatory geography that Macfarlane refers to is in Britain, but, as Glenn R. Scott's map shows, the prairies, hills, and mountains of the American southwest have their own slowly eroding memory bank of old ways seamed into the ground by human feet, horses, and post wagons.



Briefly, Scott's labyrinthine explorations of trail folklore and historical cartography in Colorado also brings to mind a story published nearly five years ago in The New York Times, on an effort by Vermont's towns and cities to catalog their "ancient roads."

As the Times explained, a 2006 state law had given Vermont residents a strong incentive to rediscover their state's buried and forgotten throughways by allowing municipalities to claim them as official town lands (thus ensuring that they remain as public lands, unable to be claimed by private landowners). As a result, the Times reported, "citizen volunteers are poring over record books with a common, increasingly urgent purpose: finding evidence of every road ever legally created in their towns, including many that are now impassable and all but unobservable."

These "elusive roads"—many of them "now all but unrecognizable as byways"—are lost routes, connecting equally erased destinations. In almost all particular cases, they have barely even left a trace on the ground; their presence is almost entirely textual. They are not just lost roads, in other words, mere unstable geographies flashing in and out of county land registers. They are road that have been deterrestrialized: scrubbed from the surface of the earth.

As the Times acknowledges, "Even for history buffs, the challenge is steep: evidence of ancient roads may be scattered through antique record books, incomplete or hard to make sense of." Accordingly:

Some towns, content to abandon the overgrown roads that crisscross their valleys and hills, are forgoing the project. But many more have recruited teams to comb through old documents, make lists of whatever roads they find evidence of, plot them on maps and set out to locate them.

Like something out of the geography-obsessed poetry of Paul Metcalf—part map, part deep social history, part regional etymology for re-reading place names as the myths that they are—the descriptions found in these old municipal documents are narrative, impressionistic, and vague, perfectly in tune with what Glenn R. Scott found in Colorado.

Returning to The New York Times, for instance, these descriptions "might be, 'Starting at Abel Turner’s front door and going to so-and-so’s sawmill,' said Aaron Worthley, a member of the ancient roads committee in Huntington, southeast of Burlington. 'But the house might have burned down 100 years ago. And even if not, is the front door still where it was in 1815? These are the kinds of questions we’re dealing with.'"

As Wendel told us, these sorts of cryptic references to lost byways are not only of interest to local historians—attorneys form another interest group who consult the Denver Public Library's archives with some frequency. In Vermont, too, the Times reports that these acts of perambulatory interpretation came to be part of a much larger, although fairly mundane, attempt to end "fights between towns and landowners whose property abuts or even intersects ancient roads."

In the most infamous legal battle, the town of Chittenden blocked a couple from adding on to their house, saying the addition would encroach on an ancient road laid out in 1793. Town officials forced a showdown when they arrived on the property with chain saws one day in 2004, intending to cut down trees and bushes on the road until the police intervened.

The article here goes on to refer to one local, a lawyer, who explains that "he loved getting out and looking for hints of ancient roads: parallel stone walls or rows of old-growth trees about 50 feet apart. Old culverts are clues, too, as are cellar holes that suggest people lived there; if so, a road probably passed nearby." Think of it as landscape hermeneutics: peeling back the layers in the map to reveal a vanished landscape.


"Botanical Profile representing the Forest Trees along the route explored by Lieut. A. W. Whipple, Corps. of Top. Eng., near the Parallel of 35º North Latitude, 1853-1854." Prepared by J. M. Bigelow, M.D., Botanist to the Expedition. U.S. Pacific Rail Road Exploration & Survey, War Department.

Wendel led us on through the archive's sedimentary record of human movement across the Coloradan landscape, from a filing cabinet stuffed full of railroad timetables and accident records to an overflowing folder of newspaper clippings on Denver International Airport conspiracy theories. A mournful subsection focused on anticipatory documentation of future erasures: a gorgeous 1854 botanical profile of a proposed U.S. Pacific railway route and the business-like binders of the much more recent I-25 environmental impact assessment.



Our day in the Denver Public Library was itself a kind of lost trail, as we noted with amusement that various quirks of the building made it hard to remember which stairwell we had taken to get to a certain floor—and, thus, whether we could even access that floor or the collections Wendel Cox had in mind for us—and it became abundantly clear that even libraries have their own kind of curatorial folklore, a personal but by no means written down knowledge of where to find certain books, objects, files, or collections, what those artifacts, in turn, mean for other things encountered in the archive, and how certain narrative strands tie a library, and a landscape, together from within.

Many thanks to Myra Rich for suggesting that Venue should meet with Wendel Cox, and for making the introduction, as well as to Wendel himself, for sharing his time and knowledge so generously. This post contains a few paragraphs previously published on BLDGBLOG.
 
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