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.
Maine 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
Mineral rights are automatically included as a part of the land in a property conveyance, unless and until the ownership gets separated at some point by an owner/seller. An owner can separate the mineral rights from land by: Conveying (selling or otherwise transferring) the land while retaining the mineral rights.
Figure 1 shows a well drilled into the bedrock where it intersects several fractures that provide water to the well. The water level in the well will rise to close to the local water table level due to hydrostatic pressure even if the fracture is deep. The average depth for a drilled well in Maine is about 250 feet.
Mineral rights are ownership rights that allow the owner the right to exploit minerals from underneath a property. The rights refer to solid and liquid minerals, such as gold and oil. Mineral rights can be separate from surface rights and are not always possessed by the property owner.
There are two types of aquifers in Maine: surficial materials and fractured bedrock. In unconsolidated surficial deposits the water fills the pore spaces between the rock fragments that make up the deposits.
Ordinarily, a Maine landowner owns the land from the surface on down, unless the mineral rights have been intentionally separated from the surface ownership by legal agreement.
Maine has some of the strictest mining and water quality standards in the country, and prohibits digging for metals in open pits larger than three acres.
Precious gems such as diamonds, rubies, and emeralds are not native to Maine, but some very good semi-precious gemstones have been found here.
Maine soils usually extend no deeper than about 3 feet. A surficial geology map shows various types of glacial and postglacial sediments such as sand, gravel, and clay. These are the parent materials on which most Maine soils have developed, and in many cases they extend deeper than the zone of soil formation.
