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Filtering by: Alternative title ssim Geology of Hug Point State Park, northern Oregon Coast Remove constraint Alternative title ssim: Geology of Hug Point State Park, northern Oregon Coast Academic Affiliation Oceanography Remove constraint Academic Affiliation: Oceanography Advisor Byrne, John V. Remove constraint Advisor: Byrne, John V.

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Bathymetry and structure of San Clemente Island, California, and tectonic implications for the southern California continental borderland

Creator:

Ridlon, James Barr

Abstract:

Five lithologic units, ranging in age from Middle Miocene to Recent, are defined on the basis of continuous seismic reflection profile records. Two of the units are Miocene sedimentary and volcanic rocks that have been truncated to form a major unconformity (post-orogenic surface) related to the most recent major tectonism...

Resource Type:

Dissertation

Full Text:

. Enlows, Department of Geology, Oregon State University, Corvallis, Oregon. Special thanks are due J. R
Marine geology of Astoria deep-sea fan

Creator:

Nelson, C. Hans (Carlton Hans), 1937-

Resource Type:

Dissertation

Full Text:

Geology of Astoria Deep-Sea Fan by Canton Hans Nelson A THESIS submitted to Oregon State University
Marine geology of Astoria submarine canyon

Creator:

Carlson, Paul R. (Paul Roland), 1933-

Resource Type:

Dissertation

Full Text:

. Coast and Geodetic Survey soundings. 28 and 8 are based, were collected on cruises of Oregon State
Geology of the continental terrace off the central coast of Oregon

Creator:

Maloney, Neil Joseph

Abstract:

The continental terrace west of Oregon between 43° 50'N and 44° 40' N latitude is 50 to 55 miles wide. It consists of a continental shelf, 16 to 35 miles wide, and a continental slope, 16 to 37 miles wide. The eastern portion of the shelf is a smooth, sediment...

Resource Type:

Dissertation

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sheltered areas of the outer shelf. GEOLOGY OF THE CONTINENTAL TERRACE OFF THE CENTRAL COAST OF OREGON
Coastal landslides in northern Oregon

Creator:

North, William Benjamin

Abstract:

Landsliding is a significant contributor to continuous erosion of the 150-mile northern Oregon coast. Direct loss of land to the sea by landslides occurs along 47 percent of the coast. The remaining 53 percent has minor shifting of sand along depositional areas such as spits and dunes. These minor movements...

Resource Type:

Masters Thesis

Full Text:

. Numerous examples of this occur along the Oregon coast, e. g., Bald Point in Ecola Park, and the area

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Academic Affiliation

Oceanography[remove]5

Advisor

Byrne, John V.[remove]5

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Current results range from 1964 to 1969

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Creator

Carlson, Paul R. (Paul Roland), 1933 1
Maloney, Neil Joseph1
Nelson, C. Hans (Carlton Hans), 1937 1
North, William Benjamin1
Ridlon, James Barr1

Date

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Current results range from 1964 to 1968

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Decade

1960-19695

Degree Field

Oceanography5

Degree Level

Doctoral4
Master's1

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Doctor of Philosophy (Ph.D.)4
Master of Science (M.S.)1

Language

English [eng]5

Non-Academic Affiliation

Oregon State University. Graduate School5

Peer Reviewed

No5

Resource Type

Dissertation4
Masters Thesis1

Rights Statement

Copyright Not Evaluated5

Subject

Beach erosion -- Oregon1
Coasts -- Oregon1
Geology -- California -- San Clemente Island1
Geology -- Oregon1
Geology -- Pacific Coast (Or.)1
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