Abundant evidence prevails along the western border of California that the relation of land to sea has undergone many changes in past geologic time. The ceaseless onslaught of the continental margin by the Pacific Ocean, accompanied by a restlessness on the part of the land, has been largely instrumental in bringing about extensive invasions of the sea during the long periods of the geologic past. Commonplace though the evidence may be to the geologist, the facts that point to the former presence of the sea where now exists only dry land are sometimes startling in their revelation to the layman
The Ventura region is of interest for its great thickness of Tertiary sediments, and for the nearly ...
journal article; BookCalifornia is along the western borderland of North America where sedimentary d...
Shepard has made us familiar with the shape and various properties of submarine gorges and in a numb...
Abundant evidence prevails along the western border of California that the relation of land to sea h...
In passing from the Jurassic to the Lower Cretaceous North America underwent but little change along...
Recognition of geologic features and processes by the peoples of southern California dates back at l...
Some of the striking fossil remains dating from the Age of Mammals that have come to light in the ro...
In comparison with the eastern half of North America, great topographic changes have occurred, in th...
Alluvium disposed along the margins of the land occupies a position of\ud special interest to studen...
Highly fossiliferous marine sediments of Cenozoic age are widely distributed in the coastal parts of...
The floor of the ocean off southern California consists of a\ud series of low depressions and basins...
This study seeks to examine patterns of longterm sediment movement along a portion of the California...
Western California between the 37th and 40th parallels is part of an active mobile orogenic belt in ...
Remains of land mammals occurring in Tertiary formations of the Pacific Coast marine province of wes...
Modern southern California is fragmented by faults that juxtapose blocks with contrasting topographi...
The Ventura region is of interest for its great thickness of Tertiary sediments, and for the nearly ...
journal article; BookCalifornia is along the western borderland of North America where sedimentary d...
Shepard has made us familiar with the shape and various properties of submarine gorges and in a numb...
Abundant evidence prevails along the western border of California that the relation of land to sea h...
In passing from the Jurassic to the Lower Cretaceous North America underwent but little change along...
Recognition of geologic features and processes by the peoples of southern California dates back at l...
Some of the striking fossil remains dating from the Age of Mammals that have come to light in the ro...
In comparison with the eastern half of North America, great topographic changes have occurred, in th...
Alluvium disposed along the margins of the land occupies a position of\ud special interest to studen...
Highly fossiliferous marine sediments of Cenozoic age are widely distributed in the coastal parts of...
The floor of the ocean off southern California consists of a\ud series of low depressions and basins...
This study seeks to examine patterns of longterm sediment movement along a portion of the California...
Western California between the 37th and 40th parallels is part of an active mobile orogenic belt in ...
Remains of land mammals occurring in Tertiary formations of the Pacific Coast marine province of wes...
Modern southern California is fragmented by faults that juxtapose blocks with contrasting topographi...
The Ventura region is of interest for its great thickness of Tertiary sediments, and for the nearly ...
journal article; BookCalifornia is along the western borderland of North America where sedimentary d...
Shepard has made us familiar with the shape and various properties of submarine gorges and in a numb...