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The Brothers Fault Zone High Lava Plains The John Day Country

Edgar Hayes

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Central Oregon Geology: The Brothers Fault Zone, High Lava Plains, & the John Day Country

by William Szary

4.6 out of 5

Language	:	English
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The Brothers Fault Zone High Lava Plains The John Day Country is a stunning and diverse region of central Oregon. It is home to a wide variety of geological features, including the Brothers Fault Zone, the High Lava Plains, and the John Day Country. These features are all part of the larger Columbia River Plateau, which was formed by a series of volcanic eruptions that occurred over millions of years.

The Brothers Fault Zone is a major geological feature that runs through the center of the region. It is a series of faults that have created a series of uplifted and downthrown blocks. These blocks have created a variety of landforms, including mountains, valleys, and plateaus.

The High Lava Plains are a high desert region that lies to the east of the Brothers Fault Zone. They are covered in a thick layer of lava that was erupted from a series of volcanoes that were active in the Miocene epoch. The lava flows have created a variety of landforms, including lava tubes, cinder cones, and lava domes.

The John Day Country is a region of badlands that lies to the west of the Brothers Fault Zone. It is home to a variety of fossil beds that have yielded a wealth of information about the plants and animals that lived in the region during the Miocene epoch. The John Day Country is also home to a number of Native American sites, including the Painted Hills and the John Day Fossil Beds National Monument.

The Brothers Fault Zone High Lava Plains The John Day Country is a region of great geological and natural beauty. It is a must-read for anyone interested in the geology and natural history of the Pacific Northwest.

The Brothers Fault Zone

The Brothers Fault Zone is a major geological feature that runs through the center of the Brothers Fault Zone High Lava Plains The John Day Country. It is a series of faults that have created a series of uplifted and downthrown blocks. These blocks have created a variety of landforms, including mountains, valleys, and plateaus.

The Brothers Fault Zone is about 100 miles long and 20 miles wide. It is bounded by the Cascade Range to the west and the Blue Mountains to the east. The fault zone is named after the Brothers, a pair of mountains that are located in the center of the fault zone.

The Brothers Fault Zone is a relatively young geological feature. It formed during the Miocene epoch, about 10 million years ago. The fault zone is the result of the collision between the North American Plate and the Pacific Plate. The collision caused the North American Plate to be uplifted, which created the Brothers Fault Zone.

The Brothers Fault Zone is a major geological feature that has had a significant impact on the landscape of the Brothers Fault Zone High Lava Plains The John Day Country. The fault zone has created a variety of landforms, including mountains, valleys, and plateaus. The fault zone has also been a source of volcanic activity, which has created a variety of volcanic features, including lava tubes, cinder cones, and lava domes.

The High Lava Plains

The High Lava Plains are about 100 miles wide and 200 miles long. They are bounded by the Cascade Range to the west and the Blue Mountains to the east. The High Lava Plains are a relatively flat region, with an average elevation of about 4,000 feet.

The High Lava Plains are a sparsely populated region. The only major town in the region is Burns, which has a population of about 3,000 people. The High Lava Plains are home to a variety of wildlife, including pronghorn antelope, mule deer, and coyotes.

The High Lava Plains are a popular destination for recreation. The region offers a variety of opportunities for hiking, camping, fishing, and hunting. The High Lava Plains are also home to a number of hot springs, which are a popular destination for relaxation.

The John Day Country

The John Day Country is about 100 miles wide and 200 miles long. It is bounded by the Cascade Range to the west and the Blue Mountains to the east. The John Day Country is a relatively dry region, with an average annual precipitation of about 10 inches.

The John Day Country is a sparsely populated region. The only major town in the region is John Day, which has a population of about 1,800 people. The John Day Country is home to a variety of wildlife, including pronghorn antelope, mule deer, and coyotes.

The John Day Country is a popular destination for recreation. The region offers a variety of opportunities for hiking, camping, fishing, and hunting. The John Day Country is also home to a number of hot springs, which are a popular destination for relaxation.

Central Oregon Geology: The Brothers Fault Zone, High Lava Plains, & the John Day Country

by William Szary

4.6 out of 5