The Underworld of Oregon Caves National MonumentContor, Roger J.
Science
The Underworld of Oregon Caves National Monument
Contor, Roger J.
Oregon Caves National Monument (Or.)
Joint
A crack, which in limestone forms at an angle to a bedding plane.
A series of joints often intersect each other in a four-sided
pattern.
Limestone
A rock consisting chiefly of calcium carbonate, usually an
accumulation of organic remains such as shells.
Marble
Limestone crystallized by metamorphism.
Metamorphose
To change into a different form, such as changing sedimentary rock
(limestone) into a metamorphic rock (marble).
Moonmilk
A rare form of hydromagnesite or calcium carbonate which is
semisolid.
Phreatic zone
The region, below the water table, in which rock is saturated with
water.
Popcorn
Nodules of mineral deposits formed in such a way as to resemble
popcorn.
Rimstone
A calcite deposit around the edge of a pool of water.
Sedimentary rock
Formed from deposits of sediments or from fragments of other
minerals.
Shale
A sedimentary rock formed from deposits of clay or silt.
Solution
The process by which a substance is chemically combined with a
liquid. Also, the state of being chemically so combined.
Soda straw
A small, hollow stalactite inside which drops of water descend.
Speleogen
A cave feature produced by solution of base rock.
Speleologist
One who makes a scientific study of caves.
Speleology
The scientific study of caves in all their aspects.
Speleothem
A cave feature produced by deposition of mineral.
Spelunker
One who explores caves as a sportsman or amateur speleologist.
Stalactite
A calcite speleothem which grows downward, icicle-fashion, as a
result of deposition by dripping water.
Stalagmite
A calcite speleothem which grows upward from a cave floor as a
result of deposition by dripping water.
Vadose zone
The region lying between the surface of the earth and the water
table. Water which seeps or flows through this region under the
pull of gravity is called vadose water.
Water table
The meeting place of the phreatic and vadose zones. Below it, the
rock is saturated with water; above it, water under the pull of
gravity is continuously flowing downward.
SUGGESTED READING
Davidson, E. J., “History of the Discovery of the Marble Halls of
Oregon.” _Oregon Historical Quarterly_, Vol. 23, pp. 274-276
(1922).
Folsom, Franklin, _Exploring American Caves_. New York, Crown
Publishers, Inc., 1956.
Halliday, William R., _Adventure Is Underground_. New York, Harper and
Brothers, Publishers, 1959.
Mohr, Charles E., and Howard N. Sloane, _Celebrated American Caves_. New
Jersey, Rutgers University Press, 1955.
Wells, Francis G., Preliminary geological map of southwest Oregon.
U.S.G.S. Mineral Investigation Map, MF 38, 1955.
_RULES AND REGULATIONS_
(_Briefed_)
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account