The Naturally Occurring Radium, Thorium, Or Other Materials (“Norm”) form, the assignee has inspected the assets for the purpose of detecting the presence or concentration of naturally occurring radium, thorium, and other such materials (“NORM”) and satisfied itself as to their physical and environmental condition, both surface and subsurface, and Assignee accepts all of the same.
California Naturally Occurring Radium, Thorium, Or Other Materials
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Multi-State
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US-OG-500
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FAQ
Thorium is a naturally occurring radioactive metal that is found in soil, rock, and water. It is formed by the radioactive decay of uranium. Minerals such as monazite, thorite, and thorianite are rich in thorium and may be mined for the metal.
The radioactivity of uranium affects the minerals around it. If you are examining a pegmatite, these signs of uranium include blackened fluorite, blue celestite, smoky quartz, golden beryl and red-stained feldspars. Also, chalcedony that contains uranium is intensely fluorescent with a yellow-green color.
Uranium is found in: Drinking water sources in some places, such as parts of the Central Valley and some areas of Southern California. Some foods, such as root vegetables and leafy greens, grown in areas containing uranium in soil or water.
Radium is a naturally-occurring metal that is almost ubiquitous in soils, water, geologic materials, plants, and foods at low concentrations. The utilization of radium, uranium, and fossil fuels has resulted in the redistribution of radium in the environment by way of air, water, and land releases.
Naturally occurring radioactive material (NORM) is found in the environment and contains radioactive elements of natural origin. NORM primarily contains uranium, thorium and in some cases potassium. Even though uranium and thorium occur naturally, by statute and rule they are defined as source material.
The following rock units contain uranium in concentrations above the crustal average: the Monterey Formation, asphaltic rocks, marine phosphatic rocks, granitic rocks, felsic volcanic rocks, and certain metamorphic rocks.
Uranium-bearing columbate, tantalate, or titanate minerals have been reported from pegmatite and granitic rock in southeastern and eastern California.
The states with the largest known uranium ore reserves (not counting byproduct uranium from phosphate) are (in order) Wyoming, New Mexico, and Colorado.
