By Guest Blogger, Richard Heathcote, Geologist
Hello, everyone. I was asked, and readily agreed, to write a blog for Whiterock Conservancy during this ecologist interregnum. My expertise is geology, so I’ll write mainly about the substrate at Whiterock on and in which ecology happens.
The thing I find most intriguing about the place is the history of landscape development. The pre-Illinoian glaciers deposited tills over the region before about 500,000 years ago, during the Pleistocene Epoch of the Quaternary Period. The terrain of the glacial deposits then underwent erosion and alluviation for several hundred thousand years until about 55,000 years ago when strong westerly winds began depositing loess over the landscape. About 15,000 years ago, the Wisconsinan glaciation overrode the loess and pre-Illinoian tills and reached the line currently represented in this area by the Middle Raccoon River. The glacial deposits from that advance are known as the Des Moines Lobe, and the noticably high ground north of the river is the Bemis end moraine from that glacial episode. The Pleistocene epoch came to a close 10,000 years ago as the Wisconsinan glacier melted away. The succeeding and current epoch is known as the Holocene.
At the dawn of the Holocene Epoch, the Whiterock landscape was split by the Middle Raccoon River that was moving meltwater and sediment from the Des Moines Lobe. Some portion of sediment was also contributed from the pre-Illinoian till and Wisconsinan loess deposits south of the river. The river was cutting its valley south of the Bemis Moraine, and side drainages were developing into terrains north and south of the river. That activity did not progress at an even pace, rather it went in episodes alternately dominated by down cutting and sediment deposition.
Deposition along a stream occurs in the channel and on the flood plain. One characteristic of flood plains is their nearly horizontal upper surfaces. When subsequent down-cutting by the stream occurs, remnants of the flood plain remain at points along the valley. These features are called terraces. In the sequence of deposition and down-cutting in a valley, the older terraces are found at higher elevations, and younger terraces at lower elevations, down to the current level of the flood plain.
The history of Holocene alluviation and valley development of the Middle Raccoon River is contained in the terraces formed along the river itself and in the side valleys. As yet, this history has not been worked-out for the Whiterock area, but the evidence to do so is obvious and beckons a researcher to undertake the survey. The photo below was taken in Long Creek Hollow and shows Susan Heathcote standing on the floodplain of Long Creek, with an older terrace visible at about twice her height behind her, and an even older, higher terrace visible among trees to the upper right. The ages of these terraces and their relation to deposition and erosion of the river valley are key elements in determining the natural history of this landscape and of the Middle Raccoon River valley.
Bonus information: In August of this year, an impromptu, self-appointed committee met on the porch at River House and acknowledged the need to name certain geographic features at the east end of the property for future reference in trail development and geological discussion. These features are 1) the stream north of the Middle Raccoon in section 19 whose valley first trends northerly, then bends northwesterly and rises to an origin near the Oak Ridge facility (See A). This is now named Red Oak Creek (See B). 2) the stream that is tributary to Red Oak Creek and whose valley trends northward along the east side of sections 19 and 18. This is now named Earl Lee Creek (See C).
I look forward to receiving your comments on this blog, and I’ll have another offering in October. You can contact me by email here: rcheathco@aol.com.



















