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.
Indiana Geophysical and Seismic Operations
Category:
State:
Multi-State
Control #:
US-OG-800
Format:
Word;
Rich Text
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FAQ
The age of Indiana's bedrock that breaks the surface ranges between 450 million and 300 million years old. The Ordovician shale and limestone that occur as outcrops in the southeastern part of the state contain many fossils.
Yet, going from east to west across southern Indiana, the ages of various rock layers at the surface vary by about 150 million years. That corre- sponds to a vertical accumulation of sedimentary rock of 7000 feet.
In Indiana, bedrock is exposed only in the south-central part of the state and along some major rivers. In the northern half of the state, the bed- rock is in places covered by more than 400 feet of glacial till, sand, gravel, and clay.
In the northwestern part of the county, the bedrock is covered by as much as 300 ft of glacial material ; to the south the glacial materials thin and bedrock lies 60 to 80 ft below the surface in much of southern Allen County.
All of Indiana's bedrock is made of sedimentary rock that formed approximately 480 to 300 million years ago. The oldest rocks were deposited during the Ordovician Period, while the youngest rocks were deposited during the Pennsylvanian Period.
Indiana's limestone bedrock formed 570 - 245 million years before the present. During this time, our continent was much further south, closer to the equator. Temperatures were warmer, and the area was covered by a shallow ocean. The shallow ocean was filled with clams, snails and other animals.