The original purpose of this study was a detailed structural analysis of the Jurassic Otter Point Formation in order to determine if the Canyonville Fault Zone, which forms the northern boundary of the Klamath Mountains in the Riddle - Canyonville area (Benson and Perttu, 1980), extends westward to the coast and, if possible, to characterize the structure of the Otter Point Formation. Further, a detailed examination of the structural and stratigraphic relationships between the Otter Point Formation and the Eocene Roseburg and Lookingglass Formations was to be performed in an attempt to determine the tectonic history of the area
Graduation date: 1988Presentation date: 1987-10-16Eight Tertiary sedimentary and volcanic units crop...
Graduation date: 1969The thesis area is located in the southeastern corner of Harney County, Oregon....
This study examines the geologic and tectonic history of the westernmost lithotectonic belt of the K...
The Floras Creek area, east of the town of Langlois, near the southwest Oregon coast, includes Coleb...
A major change in sedimentary and structural style occurs in Eocene strata exposed along the souther...
The Galice Formation is a thick, turbiditic flysch sequence that depositionally overlies the Josephi...
Information published in U.S.G.S. Professional Papers 445 and 478 indicated to the writer that the s...
Graduation date: 1991Plate 1 dimensions: 64" x 23"\ud Plate 2 dimensions: 43" x 17"The Corvallis fau...
This study examines the geologic and tectonic history of the westernmost lithotectonic belt of the K...
The Elkhorn Ridge Argillite exposed in the Bourne-Sumpter area of eastern Oregon is a broken formati...
This study examines the geologic and tectonic history of the westernmost lithotectonic belt of the K...
This study examines the geologic and tectonic history of the westernmost lithotectonic belt of the K...
The western Jurassic belt of the Klamath Mountains is an ideal locale for the study of ophiolite gen...
This study examines the geologic and tectonic history of the westernmost lithotectonic belt of the K...
Graduation date: 1981The Middle and West Forks of Little Sheep Creek in the southern Tendoy Range ha...
Graduation date: 1988Presentation date: 1987-10-16Eight Tertiary sedimentary and volcanic units crop...
Graduation date: 1969The thesis area is located in the southeastern corner of Harney County, Oregon....
This study examines the geologic and tectonic history of the westernmost lithotectonic belt of the K...
The Floras Creek area, east of the town of Langlois, near the southwest Oregon coast, includes Coleb...
A major change in sedimentary and structural style occurs in Eocene strata exposed along the souther...
The Galice Formation is a thick, turbiditic flysch sequence that depositionally overlies the Josephi...
Information published in U.S.G.S. Professional Papers 445 and 478 indicated to the writer that the s...
Graduation date: 1991Plate 1 dimensions: 64" x 23"\ud Plate 2 dimensions: 43" x 17"The Corvallis fau...
This study examines the geologic and tectonic history of the westernmost lithotectonic belt of the K...
The Elkhorn Ridge Argillite exposed in the Bourne-Sumpter area of eastern Oregon is a broken formati...
This study examines the geologic and tectonic history of the westernmost lithotectonic belt of the K...
This study examines the geologic and tectonic history of the westernmost lithotectonic belt of the K...
The western Jurassic belt of the Klamath Mountains is an ideal locale for the study of ophiolite gen...
This study examines the geologic and tectonic history of the westernmost lithotectonic belt of the K...
Graduation date: 1981The Middle and West Forks of Little Sheep Creek in the southern Tendoy Range ha...
Graduation date: 1988Presentation date: 1987-10-16Eight Tertiary sedimentary and volcanic units crop...
Graduation date: 1969The thesis area is located in the southeastern corner of Harney County, Oregon....
This study examines the geologic and tectonic history of the westernmost lithotectonic belt of the K...