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Welcome

The purpose of this site is to share some of my recreational interests, trip reports, and plans with my family and friends, and to provide links to related resources on the web.

Click on a link to the left to explore the contents of this site. Please send your comments, corrections, or additions to webmaster1@glassmountains.com.

Why "GlassMountains"?

My home is the city of Bend located in the Deschutes Basin of Central Oregon, USA. The young High Cascades volcanoes lie to the west. The recent Newberry Volcano on the west end of the active Brothers Fault zone lies to the south. The older rhyolite domes and vents of Powell Butte and Smith Rock State Park lie to the east and north, respectively. Bend is surrounded by lava flows, cinder cones, calderas, and volcanoes, and is built upon basalt flows in a high desert environment.

Nearby lava flows are rich in obsidian, a dense and typically black volcanic glass used by many native cultures to make arrowheads and blades, and pumice, a light, porous volcanic rock that consists of a network of gas bubbles frozen amidst fragile volcanic glass and minerals.

Because of the volcanic nature of the local geology, and my interest in hiking, mountain biking, skiing, and climbing within this environment, I chose "GlassMountains" for my domain. There is no association with the Glass Mountains of West Texas, Northwestern Oklahoma, or the Eastern Sierra Nevada, California.

Bend, Oregon forecast

References:

Welcome to Bend, Oregon
Cascades Volcano Observatory
USGS Volcano Hazards Program
Deschutes and Ochoco National Forests Geology
Central Oregon Audubon Society
The High Desert Museum

17019
visitors since December 1, 2002.

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This website Copyright © 2001 Paul J. McClellan. Full copyright details here.
Please send your comments, corrections, or additions to webmaster1@glassmountains.com