|
|

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.
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
|
|
| visitors since December 1, 2002. |
|
|