A land full of ravines and springs (more than 17 springs within what would become the city limits) was what greeted early settlers. The area around Platteville was so plush, so full of resources and places for shelter, that its hard to believe it was not a meeting ground for Native American trade and ceremony.
Below, you’ll find a copy of “Platteville Ninety Years Ago, as the Site Appeared to our Pioneers / Also Some Account of the Abundance of Water that Greeted Early Settlers” by J. H. Evans, from the January 31, 1917 Platteville Journal. Evans describes what the early settlers saw, based on his own 70 year history here and conversations with city founder J.H. Rountree and others. Since the article is a bit hard to read, I’ve also transcribed it.
Following this, you’ll find a Wisconsin State Journal article from 1962 that talks about the native gatherings that some recall being held in this area. That post is under construction now, but should be finished soon. If you’re interested in the possible mound complex that’s right here in Platteville, stay tuned.
Here’s the article:
Platteville ninety years ago, as the site appeared to our pioneers
Also some account of the abundance of water that greeted our early settlers
By J.H. Evans
Transcribed from January 31, 1917 Platteville Journal
“This blessed year of 1917 marks the ninetieth anniversary of the white man’s advent on the present site of Platteville. Emanuel Metcalf’s accidental discovery of lead near the location of the City Water Works was unquestionably the primary cause of the founding of the city of Platteville. It was far from being the ideal site of the prosperous city tht now graces the location. If the traditional history of a combination of the “Badger” and the trapper Metcalf had made the discovery of mineral about half a mile further upstream, Platteville would have been located on much better ground.
“Just imagine the appearance of the 1920 acres that now comprise the corporate limits of Platteville which greeted the eyes of the pioneers who came here in 1827. The topographical features then were very different from that which meets the eye of the present dweller. At that time the site was covered with a dense forest of heavy timber, principally different kinds of oak, linn, and aspen, with a thick undergrowth of crab-apple, sumac, and briers. The site was traversed by a series of low abrupt ridges, generally running from North and North-west to the South and South-East. Many of these ridges had an altitude from four to six feet higher than at present, while the intervening ravines in nearly every instance had many springs of running water and often swamps where horses and cattle were occasionally mired. Probably there was no other place of like area better supplied with living spring water.
“To give an idea of the abundant supply of water, I will try to locate some of the principle springs which had something to do with fixing the homes of the early settlers. Most of these springs have disappeared through the effects of mining and the filling of smaller ravines.
“The Rountree spring came from a ledge of rock in the ravine which crossed Pine Street, and on the northwest corner of the lot now owned by Prof. McGregor. This spring did not have a strong flow of water, but it was important from the fact that it caused the location of Maj. Rountree’s log cabin, that being the first house built in Platteville. After the flow of water ceased, Rountree built on the site the first ice house in Platteville. Much filling has raised the grade several feet.
“The next most important spring was the ‘Vineyard Spring,’ located on the lot now owned by Rev. William Waters about eighty feet East of the present line of Water Street. This spring had a large flow of water. J.R. Vineyard built a commodious spring-house with a projecting portico over the spring on the north side. His dwelling of frame stood near the present site of the home of A. Kies. Further up this ravine were several springs, notably those of Samuel Pross and Frank Rowe. Below the Vineyard springs were other springs, those of Mrs. Nettie, Judge S.O. Paine and L.L. Goodell being best remembered. Crossing Main Street, a copious flow of water came out on a lot where the livery stable now stands. This was known as the Poersh spring, belonging to a man of that name who followed the vocation of “soap-maker.” Further south and on the west side of the ravine was a fine flow of water known as the “Hawley spring” now the property of Meyer lumber company. This spring is probably inexistence at this time.
“This ravine was a noted land-mark in early times, north of Main Street it was a boggy marsh covered with a scrubby growth of timber and brush. On the east side (of Carl’s addition), the principle raines of lead were located. At Main Street, there was a greater flow of water than at this time. This was crossed by a low wooden bridge at least fifteen feet below present grade. The apex of the ridge near the High School, and the ridge crossing Main Street between Oak and Second Streets being from four to eight feet higher than present grade made the crossing in the ravine so difficult that teams were often compelled to double in order to effect a passage.
“A spring much used in early times was located in a small ravine traversed by Prof. Williams. It served for a few years for the stables of Maj. Rountree, failing in a few years it was replaced by a well. Another spring remembered by early settlers came to the surface in the ravine which beads near the former home of W.H. Oettiker. It disappeared many years ago, long before the land was cleared by the heavy growth of timber.
“A notable spring of early times was located almost exactly under the southwest corner of the City Hall. It was on the north side of the ravine which headed near the north-west corner of the Public Square. This ravine was narrow and quite deep. So deep where it crossed Main Street between the Hendershot building and the Lumber and Fuel block, the original grade was at least ten feet below present grade. Here a small wooden bridge was built across the little stream.
“West of the city along the marshy ravine which headed near the present Fourth street there were many springs. First in order was the Hardnocks, then came the Doesher spring which afforded water for the cows in pastures as late as ten years ago. On the Grindell property, a spring for a time furnished water for the manufacture of brick. Further west on the H.S. Rountree lot there was a spring with a large flow furnishing abundant water for stock. Near this spring the village boys of 60 years ago (screened by abundant timber) had built a dam to impound water for a ‘swimming hole.’ For a few seasons this afforded the kids a fine bathing pool. Just on the south of Adams street, on a lot now owned by the E. H. Doescher estate, there was a spring notable in early times as a camping place of emigrants and gypsies. Further down the ravine there were springs on the Shepherd lot, the Oudyn lot, the Charles Nye lot, the Homer Perry lot, and the Carsten lot. Doubtless there were others. Some may yet continue to flow, but most of them have been drained by the shafts sunk for mining. Along the ridge running west from the Camp grounds, water seemed to be near the surface. Miners were troubled with water, but the intensive digging and clearing the timber finally drew off the water. The last spring on the Anthony Sherpherd lot disappeared a few years ago.
“Note: I have not attempted to name all the springs which furnished great abundance of water to our early settlers. My recollection goes back over seventy years. Some of the data here given has been gathered from our early pioneers; notably Major Rountree, J.R. Vineyard, Frederick Hollman, Samuel Moore and others. I thought a record of these matters concerning the topography of our city should be preserved.”
While researching “Indian Park,” we learned that some residents at the turn of the last century recalled their being *a* multi-day Native American gathering in that park, though no one recalled, or perhaps knew at the time, the reason for the gathering. We’ve speculated that it concerned the mound(s) that we think were more visible in the park when it was a hilly spring-fed area known as “Hill Cemetery” or “Hill Graveyard.” Kristal Prohaska located the article below in the Wisconsin State Journal. In 1962, someone recalled enough to tell the reporter that native people from “miles around congregated there once a year for a pow-wow. They always gathered under a big oak tree for their ceremonials and it is assumed they moved the grapes [graves?!] during one of these times, since they stopped returning rather abruptly.”