Libby Flats

The "Billings Tree" from his 1969 paper. The caption reads "Fig. 4. Site of 1809 fire on South Libby Flats, Medicine Bow Mts., showing trees killed by fire and replacement of forest by mesic tundra. Elevation: 3,200 m. 1 August 1967."

In the fall of 1997, I helped Bill Reiners teach a seminar at the University of Wyoming for about 15 graduate and undergraduate students.  Our goal was to learn something about the ecology of a high plateau in the Medicine Bow Mountains which is about an hour from campus.  Libby Flats is near treeline at an elevation of about 9500 feet, and  is scattered with hundreds of large, dead trees, mostly fallen but some still standing.  At several places on the plateau, stands of living Engelmann spruce had ordered themselves into ribbon forests, with parallel rows of trees separated by mostly treeless alpine vegetation.  In 1969, Dwight Billings published a paper in Vegetatio about Libby Flats, and there was still some interest in learning more about the dramatic patterns of living and dead trees there.

The "Billings Tree" on September 13, 1997. Thirty years is but an instant up there.
Dwight Billings concluded that many of the dead trees at Libby Flats had been killed by a fire in 1809.  This was based on the date of a scar in a living spruce from which he collected a cross section.  The photo above is a figure from the 1969 paper.  Here is what billings wrote about this:

“…We cut down one of these living trees to date the fire.  Instead of only one fire, there were two fires; both pre-date the coming of European man.  One occurred in 1766 and was probably a ground fire; the second fire in 1809 was apparently a severe crown fire and destroyed most of the forest.  After almost 160 years, the dead trees and logs still remain.”

The trunk of the "Billings Stump," a live, scarred tree felled by Billings in 1967.

On September 13, 1997, two students and I found the large dead spruce in Billings’ photograph.  We repeated the photo (with the first digital camera I ever used), and took two increment cores of the still solid trunk.  We also stumbled upon the cut stump of the live scarred tree that Billings had felled 30 years earlier.  The trunk was on the ground where it had fallen, and the stump was solid enough to collect a new section from it on a later visit.  I used these samples in the seminar to demonstrate some of the common applications of dendrochronology.
The Billings Stump in 1997 with two fire scars

We collected cores or sections from a couple dozen other living and dead spruce trees, some with fire scars, and along with some spruce cores from a few miles to the north built a robust ring-width chronology.  This allowed us to use cross-dating to determine the life span of dead trees and the exact year of events recorded by scars. I haven’t found those tree ring data yet, but I did find some PowerPoint files which told this story (after editing my Windows registry to allow opening old ppt files).
Click images to enlarge
Four cross-dated series from a cross-section of the Billings Stump with two scar dates. The tree was killed in 1967.

The chronology of inner dates, outer dates, and scars from the Billings Grove. Each dashed line represents the lifespan of a tree as recorded by its rings.

Cross-dated series from the Billings Tree indicate that it died in the early 1870s.

Locations of trees sampled in the Billings Grove.
We confirmed Billings’ conclusion that there was a fire in 1766 and another one in 1809 (actually, cross-dating indicates that the outer scar on the Billings Stump was made in 1810, but he got the earlier one right).  However, the dates of several other fire scars did not match either of these dates, or each other. No two of the scars we dated were formed in the same year. There is no evidence from fire scars that the 1810 fire, or any other fire, had been a stand-replacing fire. It looked like trees had been scarred by very local fires, each one of which recorded a different lightning strike (in a different year). I don’t remember how many fire scars we dated — there are only six scarred trees in the figure here.

Cross-dating the cores of the Billings Tree indicates that it died in about 1873, a time not recorded in any of the fire scars we found. There is not much evidence from outer ring dates that many of the dead trees we sampled died synchronously, for example in a fire. But there does appear to be some synchrony of tree initiation in the 1660s. That is the only evidence we found of a widespread stand initiation event. The Billings Tree may be a member of this cohort.

We were all very puzzled by the lack of synchrony among scar dates. The scars were generally convincing “cat face” scars typical of damage by surface fires. I guess it is possible that some of them were caused by bears or porcupines or falling trees. Humans seem like an unlikely agent. If they are indeed fire scars, I assume individual lightning strikes causing small fires is as good an explanation as any.

I’m rather glad that we don’t really know the answer. I like the idea that the University of Wyoming has been right down the road for 125 years, and Libby Flats still offers a challenge to those who think they understand how mountain landscapes work.

The figure at left has the locations of the trees sampled for this exercise. The current image in Google Earth suggests that the Billings Tree is still standing. Here is a KMZ file with a placemark for the tree.

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