The surface bedrock of most of the Allegheny Plateau landscape region in New York state is predominantly from the Devonian period, which occurred approximately 419-359 million years ago. This bedrock consists mainly of sedimentary rocks like shale, sandstone, and limestone, which were deposited during this geologic time period.
In areas of high elevation, the bedrock type is often metamorphic or igneous due to the intense pressure and heat associated with mountain-building processes. The age of bedrock in high elevation areas can vary widely, but it is typically older due to the long history of geologic activity that has shaped these landscapes.
The surface bedrock of Grand Island, located in the state of Michigan in the United States, was formed during the Precambrian time period. This bedrock consists primarily of ancient metamorphic and igneous rocks that date back over a billion years.
A fossil that is likely to be found in the same age bedrock as Centroceras is a marine organism such as other types of algae, foraminifera, or marine invertebrates like brachiopods or ammonites. These organisms lived in similar environments and time periods as Centroceras, making them common in the same age bedrock layers.
The bedrock in the Adirondack Mountains of New York is primarily Precambrian in age, ranging from about 1.2 billion to 1 billion years old. It is one of the oldest rock formations in North America.
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The bedrock around Syracuse is estimated to be around 380 million years old, belonging to the Devonian period. This age is based on geological studies and dating of the rock formations in the area.
The surface bedrock of most of the Allegheny Plateau landscape region in New York state is predominantly from the Devonian period, which occurred approximately 419-359 million years ago. This bedrock consists mainly of sedimentary rocks like shale, sandstone, and limestone, which were deposited during this geologic time period.
Tug Hill Plateau and St. Lawrence Lowlands
Syracuse
In areas of high elevation, the bedrock type is often metamorphic or igneous due to the intense pressure and heat associated with mountain-building processes. The age of bedrock in high elevation areas can vary widely, but it is typically older due to the long history of geologic activity that has shaped these landscapes.
The current geologic age is referred to as the Holocene epoch.
R. P. Volkmann has written: 'Preliminary bedrock geologic map, Holliston quadrangle'
Geologic column is an ordered arrangement of rock layers that is based on the relative age of the rocks. Geologic time is the time IN the geologic column.
Ice Age Floods National Geologic Trail was created in 2009.
The majority of bedrock in the Catskills was formed during the Devonian Period, which is part of the Paleozoic Era. This bedrock consists of sedimentary rocks like sandstones and shales, as well as igneous rocks like granites formed through tectonic and volcanic processes during this time.
The geologic age of fossil organisms, rock, or geologic features or events defined relative of each other.