south to northern California where it meets the Sierra Nevada. The Southern Cascades bioregion in California is bounded on the west by the Sacramento Valley and the Kla-math Mountains, and on the east by the Modoc Plateau and Great Basin. The bioregion encompasses the Southern Cas-cades section of Miles and Goudey (1997) and covers approx-imately 4 % (16,740 km2 [6,460 mi2]) of the area of California. Mt. Shasta and Mt. Lassen are located in this bioregion. The Cascades are geologically young and characterized by prominent volcanic peaks (some recently active) that stand above an extensive mainly basaltic plateau. In parts of the cen-tral and southern Cascades, volcanics overlie granitic and metamorphic rocks similar to those of the Klamath...
Photograph of Mount Shasta covered in snow, Siskiyou County, ca.1900-1940. Several communities of ho...
The area is located between the foot of the San Gabriel Mountains and the Santa Clara River and is ...
This paper describes the geology of an area six miles wide and 67 miles long, extending from the cre...
Photograph of a view of Mount Shasta from a nearby valley, Siskiyou County, [s.d.]. Trees can be see...
The Haskell Canyon region, located in the northeast portion of Los Angeles County, California, occup...
This geological investigation covers an area lying across the southern Santa Lucia Mountains in sout...
This paper describes the geology of an area six miles wide and 67 miles long, extending from the cre...
The Transverse Range province of southern California is an elongate geomorphic and structural unit t...
This geological investigation covers an area lying across the southern Santa Lucia Mountains in sout...
The San Andreas Rift after passing through the Cajon Pass in Southern California proceeds approxima...
Photograph of a sparse forest at the foot of Mount Shasta in Siskiyou County, 1930. Green pine trees...
The San Joaquin-Sacramento Valley, also known as the Great Valley of California, separates the Coast...
ABSTRACT\ud MAPPING VEGETATION IN CALIFORNIA???S CASCADE FOOTHILLS:\ud BIG CHICO CREEK, CHICO, CALIF...
As a tool in discriminating basic rocks from different tectonic settings, a type of diagram was deve...
The area discussed in this report lies in the southernmost part of the California Coast Ranges, dire...
Photograph of Mount Shasta covered in snow, Siskiyou County, ca.1900-1940. Several communities of ho...
The area is located between the foot of the San Gabriel Mountains and the Santa Clara River and is ...
This paper describes the geology of an area six miles wide and 67 miles long, extending from the cre...
Photograph of a view of Mount Shasta from a nearby valley, Siskiyou County, [s.d.]. Trees can be see...
The Haskell Canyon region, located in the northeast portion of Los Angeles County, California, occup...
This geological investigation covers an area lying across the southern Santa Lucia Mountains in sout...
This paper describes the geology of an area six miles wide and 67 miles long, extending from the cre...
The Transverse Range province of southern California is an elongate geomorphic and structural unit t...
This geological investigation covers an area lying across the southern Santa Lucia Mountains in sout...
The San Andreas Rift after passing through the Cajon Pass in Southern California proceeds approxima...
Photograph of a sparse forest at the foot of Mount Shasta in Siskiyou County, 1930. Green pine trees...
The San Joaquin-Sacramento Valley, also known as the Great Valley of California, separates the Coast...
ABSTRACT\ud MAPPING VEGETATION IN CALIFORNIA???S CASCADE FOOTHILLS:\ud BIG CHICO CREEK, CHICO, CALIF...
As a tool in discriminating basic rocks from different tectonic settings, a type of diagram was deve...
The area discussed in this report lies in the southernmost part of the California Coast Ranges, dire...
Photograph of Mount Shasta covered in snow, Siskiyou County, ca.1900-1940. Several communities of ho...
The area is located between the foot of the San Gabriel Mountains and the Santa Clara River and is ...
This paper describes the geology of an area six miles wide and 67 miles long, extending from the cre...