The Shadow Lake formation is a geological unit that crops out in Southern Ontario,

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and northern

Pennsylvania Pennsylvania (; ( Pennsylvania Dutch: )), officially the Commonwealth of Pennsylvania, is a state spanning the Mid-Atlantic, Northeastern, Appalachian, and Great Lakes regions of the United States. It borders Delaware to its southeast, ...

United States The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 states, a federal district, five major unincorporated territorie ...

. The shaly sections act as a caprock to

petroleum reservoir A petroleum reservoir or oil and gas reservoir is a subsurface accumulation of hydrocarbons contained in porous or fractured rock formations. Such reservoirs form when kerogen (ancient plant matter) is created in surrounding rock by the presence ...

Description

The oldest

Paleozoic The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ' ...

strata in the north Lake Simcoe area consist of the mainly siliciclastic sediments of the Shadow Lake Formation. These strata lie unconformably and sharply on the Precambrian Grenville basement, however, this basal contact is rarely exposed. The Shadow Lake Formation is poorly exposed, typically occurring in small isolated outcrops along a low escarpment capped by the more resistant carbonate beds of the overlying Gull River Formation. Trending roughly east—west across the study area and ringing Paleozoic outliers, this escarpment marks the edge of the Paleozoic outcrop belt.Armstrong, 2000, p.8 The Shadow Lake Formation consists of non-fossiliferous, red, maroon and green, poorly sorted, argillaceous, arkosic

sandstone Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) ...

s and conglomerates, arenaceous (sandy) siliciclastic

mudstone Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from '' shale'' by its lack of fissility (parallel layering).Blatt, H., and R.J. Tracy, 1996, ''Petrology. ...

s (

shale Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especial ...

s) and

siltstone Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility.Blatt ''et al.'' 1980, p ...

s, and minor argillaceous

dolomite Dolomite may refer to: *Dolomite (mineral), a carbonate mineral *Dolomite (rock), also known as dolostone, a sedimentary carbonate rock *Dolomite, Alabama, United States, an unincorporated community *Dolomite, California, United States, an unincor ...

and

limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe ...

s. These rock types are commonly interbedded and gradational with each other. The Shadow Lake Formation, originally named by Okulitch (1939) based on outcrops north of Coboconk, was redefined by Liberty (1969). Okulitch included dolomitic limestones in the top of Shadow Lake Formation, whereas Liberty assigned these strata to the overlying

Gull River Formation The Gull River Formation is a geological formation of Middle Ordovician age (Caradoc Stage), which outcrops in Ontario, Canada. Lithologically, the formation is dominated by light grey to brown limestones and greenish gray dolomites with thin shal ...

. The siliciclastic sediments of the Shadow Lake Formation are gradationally overlain by impure carbonates of the Gull River Formation. The upper contact of the Shadow Lake Formation is placed where its mainly siliciclastic sediments give way to mainly carbonate sediments (typically argillaceous dolomites) of the lower Gull River Formation. Natural weathering accentuates this contact, making it appear sharp in outcrop, whereas in drill core this contact can be difficult to pick out. In Ontario, the Shadow Lake Formation ranges from in thickness, and averages approximately in thickness. The formation also crops out in Pennsylvania, where it is unconformably overlying the Loysburg Formation.1992 - Ryder - Stratigraphic framework of Cambrian and Ordovician rocks in the Central Appalachian Basin from Lake County, Ohio to Juniata County, Pennsylvania
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USGS The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, a ...

References

Bibliography

* {{cite LSA , last=Armstrong , first=D.K , year=2000 , title=Paleozoic Geology of the Northern Lake Simcoe Area, South-Central Ontario , url=http://www.geologyontario.mndmf.gov.on.ca/mndmfiles/pub/data/imaging/OFR6011/OFR6011.pdf , publisher=Ontario Geological Survey , pages=1–47 , accessdate=2018-08-07 Geologic formations of Ontario Geologic formations of the United States Ordovician Ontario Ordovician United States Sandstone formations of Canada Shale formations Sandstone formations of the United States Shale formations of the United States Conglomerate formations Siltstone formations Seal rock formations