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.
Michigan 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
Pottery clay is mined from the Earth and ground into a powder. This powder is combined with other water and other ingredients to form what's called the clay body -- what you probably picture in your mind when you think of a potter at work.
The country's largest outcropping of jasper can be found in Ishpeming; specular hematite, quartz, tourmaline and other minerals can be found near Champion and elsewhere. The rocks west of Marquette are the ancient granites, the iron formations and the copper-bearing rocks.
Clay minerals are composed mainly of silica, alumina, and water, but they may also contain appreciable quantities of iron, alkalies, and alkaline earths. Clay is formed by the mechanical and chemical breakdown of rocks.
Iron carbonate concretions, pyrite, and thin coal beds are usually present. In general, the surface clays of Michigan can be divided into three classes: (1) morainic clays; (2) lake clays; and (3) residual clays.
Most clay minerals form where rocks are in contact with water, air, or steam. Examples of these situations include weathering boulders on a hillside, sediments on sea or lake bottoms, deeply buried sediments containing pore water, and rocks in contact with water heated by magma (molten rock).
If you're out walking when the ground is wet and the path is slippery, chances are that you're walking on clay. You can also look for clay in lakes, ponds, streams or even at the seaside in some parts of the country. You might find it at sites where road workers or builders have dug down.
Clay minerals most commonly form by prolonged chemical weathering of silicate-bearing rocks. They can also form locally from hydrothermal activity. Chemical weathering takes place largely by acid hydrolysis due to low concentrations of carbonic acid, dissolved in rainwater or released by plant roots.
Finding Clay in Alluvial Deposits Clay that is deposited by rivers or steams are called alluvial deposits. These clay deposits do not need to be near a river since the clay could have been deposited by a a river millions of years ago. Still if you want to find clay, near a river is good place to begin searching.
