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Date Permissions Signed

2-15-2018

Date of Award

Summer 1981

Document Type

Masters Thesis

Degree Name

Master of Science (MS)

Department

Geology

First Advisor

Pevear, David R.

Second Advisor

Suczek, Christopher A., 1942-2014

Third Advisor

Wodzicki, Antoni

Abstract

In the Mt. Higgins area, the Chuckanut Formation is in probable fault contact with pre-Tertiary metamorphlc rocks. The Chuckanut is over- lain by Oso volcanics (zircon fission track age of 43.2 ± 1.9 MY). A diorite body (k/At date = 53 ± 8 MY) crops out in the Granite Lake area and is thought to be intrusive into the Chuckanut. Sedimentary rocks of much of the study area are dominantly thick- bedded arkoses that are generally cross-bedded, and resemble the Chuckanut type section. Sediments cropping out along and near Deer Creek are different; black, bituminous shale is the dominant rock type, and several bentonite beds are also present. Some bentonites are only a few centimeters thick and are not lithified, whereas others are thicker, lithifled and composed of amalgamated beds, some of which are graded. Glass shards and other volcanic detritus of the air-fall tephra have altered to form K-rectorlte upon heating to 275-285°C. A mld-Eocene date of 44.5 MY was obtained by fission track dating of zircons from one of the bentonites. It is proposed that the Deer Creek area sediments were deposited in lakes and other low energy environments on a swampy floodplain. Kalkberg-type mixed-layer illlte/smectite is found elsewhere in the Mt. Higgins area, and is probably indicative of higher temperatures than those which created the K-rectorite. On Mt. Higgins, the presence of andalusite suggests temperatures near 400°C. Cordlerite-bearing sediments indicate temperatures of 500°C. Heating was a result of a large geothermal system initiated by the intrusion of the Granite Lake diorite and possibly other related intrusions, and may be associated with Oso volcanlsm. Magmatic activity may have affected the area for several million years, perhaps sporadically.

Type

Text

Keywords

Chuckanut Formation, Bentonites, Mt. Higgins

Publisher

Western Washington University

OCLC Number

1028052420

Digital Format

application/pdf

Geographic Coverage

Higgins, Mount Region (Wash.)

Genre/Form

masters theses

Language

English

Rights

Copying of this thesis in whole or in part is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this thesis for commercial purposes, or for financial gain, shall not be allowed without the author's written permission.

Cruver Bedrock Geology Map Reduced 7272144.pdf (772 kB)
Bedrock Geology of the Mt. Higgins Area, North Cascades, WA

Cruver Sample Location Map reduced 7272144.pdf (127 kB)
Sample Location Map

scruver map.pdf (761 kB)
Contact or Structure - Mapped by Jones (1959)

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