Give the man room : $b The story of Gutzon BorglumCasey, Robert J. (Robert Joseph)
General
Give the man room : $b The story of Gutzon Borglum
Casey, Robert J. (Robert Joseph)
Borglum, Gutzon, 1867-1941
When I first saw the shoulders of Rushmore I knew instinctively
that I was a doomed man. I knew that while the years and I reshaped
the mountain, I must be reshaped myself.
Once before I had something of the same intense, emotional shock.
That was when I stood in front of Stone Mountain and listened to
Helen Plane pleading with me to cut into the wall the story of Lee
and his associates.
Such thoughts passed through my mind as we lay prostrate to rest
in the sun on the top of Mount Rushmore. Here great masses of rock
of new dimensions, of greater hardness, rose above and about me. I
was conscious we were in another world. We could imagine clouds
moving over us and around us in stately dignity, or driven by
hurrying winds out of the north, or falling as rain or snow against
the chill white cliff. And there a new thought seized me--a thought
that frightened me and was to redirect me and dominate all my
carving: the scale of the mountain peak!
We were 6,200 feet above sea level--500 feet above the surrounding
cliffs. We looked out over a horizon, level and beaten like the rim
of a great cartwheel, 2,000 feet below. We had reached up toward
the heavenly bodies; we were looking at the forms removed from the
detail of earth in the valleys, with crude colossi piercing the
sky. I had worked seven years on Stone Mountain without real
consciousness of this changing relationship of lofty mountain forms
isolated in space. And it came over me in an almost terrifying
manner that I never had sensed what I was planning. Plans must
change. The vastness that I saw here demanded it.
The Rushmore elevation is the highest elevation of granite, except
near-by Harney Peak, between the Rocky Mountains and Europe. It is a
hard formation called pegmatite, peculiar to the Black Hills, and on
Rushmore it is of a finer, more even grain than that of surrounding
rocks.
Once there was a sea in this region, then rising tracts of sediments
compressed into complicated folds. At some remote time the earth’s
interior intruded upon the sedimentary folds, pushing steadily upward
beneath the surface, and so formed in time the granite batholith of the
Harney Peak region. The overload above the granite must have been of
great height before it was destroyed by erosion. It was torn down and
now lies scattered across the Bad Lands and in valleys all the way to
the sea.
There is no telling when Mount Rushmore was exposed to the sky. Dr.
O’Harra believed it to be one of the oldest mountain formations in the
world--older than the Alps or the Apennines or the Pyrenees or the
Caucasus--older, even, than the Himalayas. Said Dr. O’Harra:
Public-domain text, read in full here on John Shaqi.
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