WebThe Queenston Formation is a geological formation of Upper Ordovician age (Maysvillian to Richmondian Stage), which outcrops in Ontario, Canada (along the northern and eastern flanks of the Niagara Escarpment, as well as east of Ottawa) and New York, United States (just south of Lake Ontario).A typical outcrop of the formation is exposed at Bronte … WebOct 1, 1991 · Waters of the petroleum-bearing Clinton formation (Albion Sandstone) of eastern Ohio are highly concentrated brines with average total dissolved solids (TDS) of 250,000 ppm. Sodium, calcium, and chloride account for 97% of the TDS. Distribution of divalent metal chlorides (MCl[2]) allows inference of an up-dip paleoflow direction, …
The Clinton Sands in Canton, Dover Massillon, and …
WebThe Clinton Foundation makes a difference in people’s lives across the United States and around the world through programs and partnerships that expand economic opportunity, … WebThe Cuyahoga Formation is a geologic formation in Ohio. The age of the formation is difficult to determine, because of a lack of diagnostic fossils. Roughly, the formation dates from the Late Kinderhookian (354.8 to 350.8 million years ago) to the Middle Osagean (347.7 to 344.5 million years ago). [1] glyph in typography
Clinton Formation - Wikiwand
WebJul 6, 2015 · The Clinton Sandstone formation has been drilled in Ohio since the late 1800s–for both oil and natural gas. Sandstone is a tightly packed rock like shale, rock that requires fracking in order to effectively release the oil and gas trapped in it. Until recently, the Clinton was drilled vertically. The Clinton Group (also referred to as the Clinton Formation or the Clinton Shale) is a mapped unit of sedimentary rock found throughout eastern North America. The interval was first defined by the geologist Lardner Vanuxem, who derived the name from the village of Clinton in Oneida County, New York where several well exposed outcrops of these strata can be found. The Clinton Grou… WebJul 9, 2024 · The Clinton is one of the most economically significant petroleum systems in all of Ohio (others being the Ordovician-aged Trenton Limestone of northwestern Ohio and the Cambro-Ordovician aged Knox-Rose Run interval). Stratigraphy: crack samples of talus derived from the Brassfield Formation, Llandoverian Series, Lower Silurian glyphipterix forsterella