North Dakota: A Guide to the Northern Prairie StateFederal Writers' Project of the Works Progress Administration for the State of North Dakota
History
North Dakota: A Guide to the Northern Prairie State
Federal Writers' Project of the Works Progress Administration for the State of North Dakota
North Dakota; North Dakota -- Guidebooks
Here and there, standing out against the lighter coloring of the sands
and clays, are black veins of lignite. Ages ago dense forests, rivaling
those of the tropics of today, rose over the swamps of the receding
seas. The motorcar speeds through a region where the giant hog, the
three-toed horse, and the saber-toothed tiger roamed among lofty trees.
The cast-off growth of the forest fell into the swamps below, where,
shut away from the air by water and mud, it turned into peat. Centuries
later the seas returned to crush it with heavy layers of shale and
clay, until pressure and heat drove out most of the volatile oils of
the wood, leaving carbon or coal. It is not surprising to find that
lignite coal has the same cellular formation as wood, and that it at
times bears the imprint of leaves or of whole trunks of trees. The
forms of stumps 15 feet in diameter have been found in the coal beds of
the State.
Lighting up the dull strata of the buttes are the ever present
pinks and reds of scoria--clay burnt into a brick-like shale by the
centuries-old fires of burning coal veins. Some of these burning
veins still exist in the Badlands, being more easily discoverable in
the wintertime, when the heat from combustion causes steam to rise.
This burning has been one of the major factors in the production of
the present Badlands topography, for as the fires have eaten into the
coal veins in the cliffs, the earth has crumbled and been carried away
by the rains and streams. These fires were an awesome sight to the
Indians, who believed the hills were on fire.
The chief agent, however, in the formation of the Badlands has been
the Little Missouri River, which centuries ago began to carve its way
down through the soft shales and sandstones with which the early seas
had covered the area. Aided by the eroding action of wind, frost, and
rain, by huge landslides, and by burning coal veins, the once swift,
always silt-laden river and its tributaries have floated away all the
age-old clays of the region except these buttes and domes piled in
indescribable confusion along the valley floor. The Indians, called the
valley "The-place-where-the-hills-look-at-each-other," and the first
white explorers, impeded in their travel, named it "bad lands to travel
through," a phrase inevitably shortened to Badlands.
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.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account