However, patches of bedrock consisting of conglomeratic sandstone, sandstone, and shale are also present, as are smaller areas of Wisconsinan Ice-Contact Stratified Drift . There are also a few patches of wetland.
32.
The surficial geology in the vicinity of Dymond Creek consists mainly of a till known as Wisconsinan Till, alluvium, Wisconsinan Ice-Contact Stratified Drift, and bedrock containing sandstone, conglomeratic sandstone, shale, and coal.
33.
The surficial geology in the vicinity of the lower reaches of East Branch Roaring Brook alluvium, Wisconsinan Ice-Contact Stratified Drift, bedrock consisting of conglomeratic sandstone and sandstone and shale, fill, and sand and gravel pits.
34.
The stratigraphy of the Southern Highland Rim is primarily composed of flat-lying limestones, dolomites, and shales, and to a much lesser extent, of cherts, siltstones, mudstones, and very fine grained to conglomeratic sandstones.
35.
This very thick conglomeratic formation, called the Poudingues de Palassou, is the indicator for the most important orogenic phase in the Pyrenean domain, the " Pyrenean Main Phase ", which was accompanied by very strong deformations and uplifts.
36.
The surficial geology in the vicinity of the stream's lower reaches mainly includes urban land heavily disrupted by cut and fill, a glacial or resedimented till known as Wisconsinan Till, and bedrock consisting of sandstone, conglomeratic sandstone, and shale.
37.
An isolated humerus, designated the paratype by Pang and Cheng, comes from a locality over 200 meters away from the type locality of " Huabeisaurus ", in a fluvially deposited sandy conglomeratic layer in the lower member of the Huiquanpu Formation.
38.
However, alluvium is present along the creek in its middle and upper reaches and there are some patches of Wisconsinan Ice-Contact Drift in the watershed, as well as a few patches of bedrock consisting of conglomeratic sandstone, sandstone, and shale.
39.
Big Rock is a glacial erratic that is part of a long, narrow ( wide ), linear scatter of thousands of distinctive quartzite and conglomeratic quartzite, which occurs only within the Gog Group and is found in the Athabasca River Valley of central western Alberta.
40.
In sharp contrast to argillaceous strata above and below it, the "'Shinumo Quartzite "'consists characteristically of beds that are red, brown, or purple sedimentary quartzites and lesser massive white, red, or purple sandstone; also conglomeratic sandstone.
