Coelophysis would mostly be found in the New York lowlands.
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Conglomerate and sandstone
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The ridges and valleys of the Newark lowlands are likely the result of past glacial activity and erosion. During the Pleistocene epoch, glaciers advanced and retreated multiple times over the region, carving out valleys and depositing sediment to form ridges. Subsequent erosion by water and ice further shaped the landscape into its current form.
What the central lowlands are depends greatly on which country or region is being discussed. In general, central lowlands would be centrally located low plains type of land.
sedimentary
Sedimentary.
The St. Lawrence Lowlands were primarily formed from sedimentary rocks including limestone, shale, and sandstone. These rocks were deposited and compressed over millions of years to create the lowlands we see today.
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The different animals that live in the interior lowlands of North America ,are animals like snakes and other different rodent type animals .
The two types of rock most commonly found as outcrops in New York State's Newark Lowlands landscape region are sedimentary rocks, particularly sandstone and shale. These rocks are a result of the region's geological history, which includes ancient river and lake deposits. Additionally, some areas may also exhibit igneous rocks, such as diabase, due to volcanic activity in the past.