HYDROTHERMAL ORIGIN OF THE CLAYS FROM THE UPPER SLOPES OF MAUNA KEA, HAWAII

Abstract--The soils of the summit region of Mauna Kea are similar to the soils of the high mountain deserts and to the soils of cold deserts. Dramatic differences, however, exist between the soils of the summit and other neighboring cones and the soils of the glaciated terrain. The soils of some of...

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Bibliographic Details
Main Author: F. C. Ugolini
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1973
Subjects:
Cones The
Cones, The
The Cones
Ice cap
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.563.1115
http://www.clays.org/journal/archive/volume 22/22-2-189.pdf

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