Stillwater, Minnesota is not the kind of place that comes to mind when thinking about good elephant country. If you've never been there, there's a bit of a drop from the top of the St. Croix Valley to the river (the map coming up will make this clear). Furthermore, Stillwater is not noted for its broad floodplain, so a proboscidean wouldn't have much space if it did come down. However, the deep valley of the St. Croix itself is of geologically recent vintage, a parting gift of the most recent ice age sending meltwater through an area marked by billion-year-old faults. This is all a long-winded way of saying that compared to today, it would have been much easier to have mammoths and mastodons wandering around the future area of Stillwater right after the ice had cleared out, only where they were wandering wouldn't have looked very much like how it looks like today.
In fact, what appears to be the first documented find of mammoth or mastodon fossils in Minnesota was made in Stillwater in 1856 (Anonymous 1860; Stauffer "1945"). The find was briefly mentioned in a description of the Minnesota Historical Society ("Already we find it its museum the remains of the first mastodon found in the State, presented by
A. [Abram or Abraham] J. Van Vorhes, esq., of Stillwater"; Anonymous 1860), but a fuller account would not be made until Newton Horace Winchell took an interest in it.
According to Winchell, who met with Van Vorhes, the find came from coarse river gravel (actually the base of a bed of fine sand 30–40 feet thick [9–12 m] according to the included stratigraphic section) "far above the present river, but within the main valley" and consisted of a single mastodon tusk (Winchell 1878). Obviously, as an isolated find there's really no way to be certain
where the tusk was when its services were no longer required by its
owner, but we take our tusks where we find them. (There
are differences between mastodon and mammoth tusks, but I don't know if these were known in the mid-1800s, or if this is just a case of "mastodon = generic American proboscidean".) Van Vorhes also reported pottery fragments at the top of the sand bed. Eight feet (about 2.5 m) of the tusk went to the Academy of Sciences of St. Paul (Winchell 1878), and would have been lost in the 1881 fire (mentioned
previously).
Winchell also included an extensive quotation from Van Vorhes, who reported multiple tusks "
were found about eight or ten feet [about 3 m]
above the base of the hill: the hill at this point rises at an angle of about 45°. After excavating in the base of the hill on the grade of Myrtle Street about 37 feet [11 m]
, the tusks were found, consequently 37 feet below the surface. At this point the hill was about 90 feet high [27 m]
.
The crockery I found some thirty feet [9 m]
farther into the hill and some six or eight feet [about 2 m]
higher in the strata. This hill is a continuous tongue of land lying between the Florence mill stream and a spring run. The two streams run parallel and some 350 feet [107 m]
apart. The hill is so steep on the Florence mill side as to be inaccessible except by clinging to roots and brush growing on it. The material at the base is sand and small gravel. Where the tusks were found the strata were pure sand ten or twelve feet thick [about 3 m]
, exhibiting clearly the direction of the current in an eastward inclination one or two degrees."
Leaving aside the question of one tusk or multiple tusks, the location of the find can be reasonably well established from Van
Vorhes’s recollections (refreshing for a mid-19th-century find!). The Florence flour mill is long gone, and
was not built until 1872, so Van Vorhes was using the then-current geography to describe the 1856 situation. However, as mentioned in the linked article, "The water for the mill was brought down from a dam located where the Pitman House once stood, now the northern portion of Trinity Lutheran Church, and supplied by a brook from McKusick’s Lake." The church is adjacent to Myrtle Street between 3rd Street N and 4th Street N, and a valley can be traced from this area to the lake. The "spring run" seems most likely to be related to a valley to the south, but the present-day distance is much greater than 350 feet. Given that Van Vorhes was an experienced surveyor, it's unlikely he would have been off by hundreds of feet or more; it seems more likely to me that the critical area has been so heavily modified in later years that the 1856 watercourses have been obscured or obliterated. My guess is that the find was made within 500 feet (150 m) of the present location of the church.
 |
| This map (helps to click) shows several of the landmarks mentioned
above. As I said, I think the find was made in the vicinity of the
modern church. (Here's a plug: I've found the Earth Point topo map overlay for Google Earth invaluable!) |
The location was retransmitted incorrectly in Hay (1924:44), who placed it in Browns Creek. I suspect this stems from a misreading of a later report by Winchell. Winchell (1888:397) stated "In the fall of 1872 the writer [Winchell] first visited Stillwater, and in company with Mr. Abram Van Vorhes examined the deposit of tripoli in the valley of Brown's Creek. At the same time Mr. Van Vorhes pointed out the drift bank in which he had found ancient pottery and the remains of the mastodon." It's not hard to see how a reader may have come to the conclusion that the "drift bank" was in Browns Creek. This creek, though, is on the north side of Stillwater; Highway 96 borrows part of its valley. It is approximately 1.4 miles (2.3 km) north of the actual area of the find.
The loss of the specimen relegated it to a paper curio. Winchell returned to it once more, in 1910, which is notable because he hedged on the mastodon identification, acknowledging it could have been an "elephant" (mammoth). Aside from Hay (1924), the only other place it seems to have appeared in the literature since Winchell is
Stauffer's inventory of Minnesota's Pleistocene fossils (usually given as 1945, but at least 1948). Winchell’s report is #17 in this publication, and Stauffer classified it as "
Elephas sp.", which translates as "some kind of proboscidean". Stauffer included another Stillwater find, #6, a tusk found in terrace gravels “in the edge of Stillwater” at an unspecified time. With such little information, it is impossible to say anything else about it.
[An unrelated closing note: I really ought to plug the
Geological Society of Minnesota more frequently for local readers; for example, there was a talk this week on Cretaceous fossils in Minnesota. This would have been the normal closing session of the spring lecture series, but an opportunity arose for the GSM to co-sponsor a presentation by Peter Brannen on "The Ends of the World", his book about extinction events, Monday, May 20th (see flyer below for more details). The fall lecture series will start up in September. The GSM staffs a booth during the State Fair in the Education building if you'd like to stop by and chat in person. Lectures are free and open to the public.]
References
Anonymous. 1860.
Minnesota. The Historical Magazine 4(5):141–142.
Hay, O. P. 1924.
The Pleistocene of the middle region of North America and its vertebrated animals. Carnegie Institute of Washington Publication 322A.
Stauffer, C. R. “1945” [at least 1948 based on dates in the article]. Some Pleistocene mammalian inhabitants of Minnesota. Minnesota Academy of Science Proceedings 13:20–43.
Winchell, N. H. 1878. Primitive man at Little Falls.
Minnesota Geological and Natural History Survey Annual Report 6:53–65.
Winchell, N. H. 1888. The geology of Washington County. Pages 375–398 in N. H. Winchell and W. Upham.
The geology of Minnesota. Minnesota Geological and Natural History Survey, Final Report 2. Johnson, Smith & Harrison, state printers, Minneapolis, Minnesota.
Winchell, N. H. 1910.
Extinct Pleistocene mammals of Minnesota. Bulletin of the Minnesota Academy of Science 4:414–422.
