This lease rider form may be used when you are involved in a lease transaction, and have made the decision to utilize the form of Oil and Gas Lease presented to you by the Lessee, and you want to include additional provisions to that Lease form to address specific concerns you may have, or place limitations on the rights granted the Lessee in the “standard” lease form.
North Dakota Surface Pits
Category:
State:
Multi-State
Control #:
US-OG-827
Format:
Word;
Rich Text
Instant download
Description
How to fill out Surface Pits?
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FAQ
In North Dakota, sedimentary rocks such as limestone, sandstone, and shale, all of which were deposited in water, lie above the igneous rocks. They formed when sediments washed into the seas that covered the state during much of the past 600 million years.
The clays of North Dakota can be grouped into three general categories: bedrock clays, glacial clays, and lacustrine clays. Since three fourths of North Dakota is covered by glacial sediments, glacial clays are the most abundant at or near the surface.
For example, an erratic could be a boulder of sandstone is picked up by a glacier, transported, and deposited on top of a limestone bedrock. Some erratics are useful to scientists because they are of a distinctive rock type, which means that their source outcrop can be identified and located.
Glaciers that moved over North Dakota left behind various kinds of erratics, rocks that would not otherwise be found in the state. Most were brought here from Canada.
A glacial erratic is a glacially deposited rock differing from the type of rock native to the area in which it rests. Erratics, which take their name from the Latin word errare ("to wander"), are carried by glacial ice, often over distances of hundreds of kilometres.
It has been estimated that North Dakota contains a mineable reserve of 480,000 pounds of U3O8 at an $8.00 per pound market price. The uranium reserves of North Dakota represent far less than 1 percent of the total U.S. reserves.
Explore PeriodFormationSedimentCretaceousHell CreekSand, Silt, Clay, SandstoneCretaceousPierreShaleQuaternaryColeharborTill (Unbedded, unosrted mixture of clay, silt, and cobbles)QuaternaryOaheClay, Sand21 more rows
These rocks are known as glacial erratics. Erratics record the story of a glacier's travels. Looking for the bedrock units that correspond with erratics can reveal complex flow patterns.
