Publication Type |
Book |
Author |
Pruitt, Robert G. Jr. |
Title |
Gilsonite |
Date |
1961-06 |
Description |
Glisonite is a black, pitch-like substance which occurs in pure form in large veins in the Tertiary sediments of the Uinta Basin. It is a homogenous petroleum substance (technically it is a predominently aromatic asphaltite) which fuses relatively easily and burns like tar. Glisonite is brittle and has a distinctive conchoidal to hackly fracture. Fresh glisonite has a brilliant black luster, but weathered glisonite and some of the more refractory varieties have a dull, soot-black appearance. Glisonite has a specific gravity of 1.07, just slightly denser than water, and a hardness of 2 to 2.5 on Moh's Scale. Glisonite is soluable in asphalt-based petroleum, and is frequently employed to change the consistency of lighter petroleum products. Finely pulverized glisonite is chocolate brown in color and exceedingly penetrating to the skin and lungs. |
Type |
Text |
Publisher |
Utah Geological and Mineralogical Survey, University of Utah, College of Mines and Mineral Industries |
Subject |
glisonite; bitumen; asphalt-based petroleum; glisonite ore |
Language |
eng |
Bibliographic Citation |
Pruitt, R. G. Jr. (1961). Gilsonite. Utah Geological and Mineralogical Survey, University of Utah, College of Mines and Mineral Industries. The mineral resources of Uintah County: Bulletin, 71(3), p. 23-49. |
Relation Has Part |
The mineral resources of Uintah County: Bulletin; no. 71, cha. 3, pp. 23-49 (1961) |
Rights Management |
(c)Utah Geological and Mineralogical Survey, University of Utah, College of Mines and Mineral Industries |
Identifier |
ir-eua/id/2942 |
Source |
DSpace at ICSE |
ARK |
ark:/87278/s69g8kx9 |
Setname |
ir_eua |
ID |
214029 |
Reference URL |
https://collections.lib.utah.edu/ark:/87278/s69g8kx9 |