Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meaningsLoomis, Frederic Brewster
Science
Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meanings
Loomis, Frederic Brewster
Minerals -- United States; Rocks -- United States
Certain sedimentary rocks contain larger or smaller quantities of
natural gas, petroleum, mineral tar and asphalt. These are compounds of
carbon and hydrogen, or hydrocarbons, and range from gases to solids,
each being a mixture of two or more hydrocarbon compounds. The crude
petroleum may have either a paraffin base or an asphalt base: in the
former case, when the gas, gasoline, kerosene, etc., have been removed
by distillation, the solid residue will be paraffin, as in most of the
Pennsylvania crude oils; while in the latter case, the solid residue
will be an asphalt, as in most of the California and Texas crude oils.
In the case of the paraffin series all the compounds belong to the
paraffin group, while the asphalt is due to the presence, in addition to
the paraffin group, of some of the benzine series of hydrocarbons.
Petroleum is found in sands and shales, which were originally deposited
on ancient sea bottoms, the shales generally being the real source of
the petroleum. The oil was once the fatty portion of animal bodies
(perhaps to some extent of plant bodies), and was separated during
decomposition as a result of bacterial activity. Oil thus produced is in
tiny droplets, which have a great affinity for clay. After being freed
by the bacteria, the oil droplets in muddy water attach themselves to
particles of clay, and as the clay settles the oil is carried down with
it, the two eventually making a bituminous shale. In clear water, or in
water which is in motion, the oil droplets rise to the surface and
eventually distill into the air.
The oil, or petroleum, may stay diffused through the shales, in which
case we have _oil-bearing shales_, with sometimes as much as 20% of oil.
Were there but ¹/₁₀₀₀ of a per cent of oil in a layer of shale 1500 feet
thick, this would amount to 750,000 barrels per square mile which is
equal to a rich production from wells. When the oil in shale amounts to
three per cent or more, it is commercially usable. There are large
stretches of petroleum-bearing rocks in New York, Pennsylvania, Ohio,
Indiana, and all the way out to the Pacific coast, some of them with oil
so abundant, that a blow of the hammer will cause them to smell of
petroleum.
Public-domain text, read in full here on John Shaqi.
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