Kentucky 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

In Kentucky, a dark-colored igneous rock, peridotite, occurs in sills and dikes (intrusions) in Elliott County in eastern Kentucky and Caldwell, Crittenden, and Livingston Counties in western Kentucky.

Throughout the Ordovician, Kentucky was covered in shallow tropical seas, depositing limestone, dolomite and shale. The region was the flooded continental shelf of Laurentia, situated in the Southern Hemisphere as part of the Iapetus Ocean, based on reconstructed paleogeography.

Swamps covered Kentucky during the ensuing Carboniferous period. From the start of the Permian to the Pleistocene, there is a large gap in the geologic record, although the gap is interrupted by minor deposits of Cretaceous and Eocene rocks, which mainly preserve plant fossils.

The original source of these igneous rocks is most likely the northern Appalachian Mountains or Canada. Other igneous rocks such as granites, basalts, gneisses, and amphibolite occur in the deep subsurface of Kentucky.

Mineral resources in Kentucky fall into four broad categories: metals, gemstones, industrial and coal, and oil and natural gas. Metals include zinc, lead, iron, copper, titanium, and rare earth elements. Pearls, diamonds, and agates are examples of semiprecious or precious gemstones.

The Landscape of Kentucky Caves, sinkholes, sinking creeks, large springs, and other features associated with underground drainage are found in the limestone terrains typical of the Pennyroyal (Mississippian Plateaus) and the Bluegrass Regions.

Stream erosion has been the predominant geological force sculpting and modifying the Kentucky landscape since the close of the Paleozoic Era. A horseshoe-shaped belt of ridges and hundreds of more or less isolated, rounded, and conical hills border the Bluegrass Region on the west, south, and east.

These mountains vary in elevation from 2,000 feet (600 metres) to 4,145 feet (1,263 metres) at Big Black Mountain, the highest point in Kentucky. The plateau is underlain by large deposits of coal, limestones used for cement, and fine-grained sandstones suitable for construction and decorative purposes.

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Kentucky Geoscience Operations on the Contract Area