known
European locality, and also from any place known in America other than
the one from which all these pipes come, and which are all traceable, I
have found, to one source, and that source as yet unvisited, except by
the red man, who described it everywhere as a place of vast importance
to the Indians, as given to them by the Great Spirit for their pipes
and strictly forbidden to be used for anything else." Specimens of the
mineral were sent to Dr. Charles T. Jackson, of Boston, who was then
"one of our best mineralogists and chemists." He gave it the name "
catlinite," and pronounced it a new mineral compound, not steatite,
harder than gypsum and softer than carbonate of lime.
This locality was visited and referred to by Dr. Charles A. White1
and subsequently described by Dr. Ferdinand V. Hayden. He says : " On
reaching the source of the Pipestone Creek, in the valley of which the
pipestone bed is located, I was surprised to see how inconspicuous a
place it is. Indeed, had I not known of the existence of a rock in this
locality so celebrated in this region, I should have passed it by
almost unnoticed. The pipe-stone layer, as seen at this point, is about
11 inches in thickness, only about 2\-1/4 inches of which are
used for manufacturing pipes and other ornaments. The remainder is too
impure, slaty, fragile, etc. A ditch from 4 to 6 feet wide and about
400 yards in length, extending partly across the valley of the
Pipestone Creek, reveals what has thus far been done in excavating the
rock."2
Longfellow's lines commemorate the Indian legend :
"
From the redstone of the quarry With his hands he broke a fragment,
Moulded it into a pipe-head. Shaped and fashioned it with figures; From
the margin of the river Took a long reed for a pipestem, With its
dark-green leaves upon it."
Whether
catlinite has been used to make pipes for any very great length of time
is difficult to decide. According to Dr. Hayden, "the quarry belongs to
a comparatively recent