A section of the Paleozoic formations of the Grand Canyon at the Bass trail

Professional Paper 131-B
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Abstract

The thick series of horizontal strata of Paleozoic age which makes the greater part of the wall of the Grand Canyon is probably broadly familiar to more people than the strata exposed in any other area in the western United States. Each detail of form or color in the wall is so definitely associated with a bed or set of beds in the series that these strata are the very elements of the canyon landscape. Consequently they have been described not only by geologists but by many writers who have been interested in the Grand Canyon chiefly as a scenic spectacle.

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Publication type Report
Publication Subtype USGS Numbered Series
Title A section of the Paleozoic formations of the Grand Canyon at the Bass trail
Series title Professional Paper
Series number 131
Chapter B
DOI 10.3133/pp131B
Year Published 1923
Language English
Description 50 p.
First page 23
Last page 73
Country United States
State Arizona
Other Geospatial Grand Canyon
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