Tennessee Geoscience Operations on the Contract Area

State:
Multi-State
Control #:
US-OG-705
Format:
Word; 
Rich Text
Instant download

Description

This form provides that any Party may propose that geoscience operations be conducted on the Contract Area lands. The Party wishing to conduct geoscience operations shall furnish the other Parties with an information notice which generally describes the proposed geoscience operation.

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FAQ

Deformation and Mountain Building As ancestral North America and Africa collided, the entire Appalachian region was uplifted, creating mountains whose elevations were likely higher than the Rockies today. Continental collisions generate huge amounts of pressure and heat, which has a number of interesting effects.

Most of the sediment across Middle Tennessee was deposited from the Ordovician to the Mississippian, roughly between 400 and 300 million years ago. The sediment was primarily deep ocean limestones with some shale layers.

The landscape formed on Paleozoic sedimentary rocks that range in age from Cambrian to Pennsylvanian, around 540 to 290 million years before the present. The ridges are composed of Pennsylvanian sandstone belonging to the Pottsville Formation, whereas the valleys cut through shale, limestone, and dolomite.

The geology of Tennessee is as diverse as its landscapes. Politically, Tennessee is broken up into three Grand Divisions: East, Middle, and West Tennessee. Physically, Tennessee is also separated into three main types of landforms: river valley plain, highlands and basins, and mountains.

Limestone is the most common bedrock in Middle Tennessee. This is found in most of the Highland Rim and Nashville Basin. However, Highland Rim limestones tend to be more siliceous and cherty, contrary to the purer limestone in the Nashville Basin.

This act of , created the Tennessee Valley Authority to oversee the construction of dams to control flooding, improve navigation, and create cheap electric power in the Tennessee Valley basin.

The Tennessee Valley is the drainage basin of the Tennessee River and is largely within the U.S. state of Tennessee. It stretches from southwest Kentucky to north Alabama and from northeast Mississippi to the mountains of Virginia and North Carolina. The border of the valley is known as the Tennessee Valley Divide.

Tennessee's natural resources include but are not limited to wildlife, forests, grasslands, fish, water, air, soils, and their interrelationships.

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Tennessee Geoscience Operations on the Contract Area