The North Fork John Day Wilderness is a wilderness area within the Umatilla and Wallowa–Whitman National Forests in the Blue Mountains of northeastern Oregon .
18-730: The wilderness consists of four separate units: the main 85,000-acre (34,000 ha) unit of the North Fork John Day drainage; the Greenhorn Unit to the south; the Tower Mountain Unit to the north; and the Baldy Creek Unit to the east. Approximately 6,000 acres (2,400 ha) of the Vinegar Hill-Indian Rock Scenic Area also lie within the wilderness. The North Fork John Day Wilderness is located within
36-559: A herd of mule deer that reportedly exceeds 150,000. Bull elk here sometimes weigh more than 800 pounds (360 kg) and sport antlers spreading beyond 5 feet (1.5 m). There are over 130 miles (210 km) of perennial streams in the wilderness, 40 miles (64 km) of which provide spawning habitat for chinook salmon and steelhead . Other wildlife in the North Fork John Day Wilderness include mountain goats and black bears . Primary recreational activities in
54-689: A variety of rock formations including basalt , rhyolite , granite , and shales can be seen here. The area has a history of mining, and active and decaying remains of mines can be seen. Motor vehicles are prohibited, except during winter when snowmobiles are allowed. A portion of the Vinegar Hill-Indian Rock Scenic Area lies within the Desolation Watershed. 44°44′N 118°38′W / 44.73°N 118.63°W / 44.73; -118.63 North Fork John Day Wilderness The North Fork John Day Wilderness
72-526: Is a wilderness area within the Umatilla and Wallowa–Whitman National Forests in the Blue Mountains of northeastern Oregon . The wilderness consists of four separate units: the main 85,000-acre (34,000 ha) unit of the North Fork John Day drainage; the Greenhorn Unit to the south; the Tower Mountain Unit to the north; and the Baldy Creek Unit to the east. Approximately 6,000 acres (2,400 ha) of
90-854: Is a high-elevation scenic area in the northeast portion of the Malheur National Forest in the state of Oregon . It provides vistas of the North Fork John Day Wilderness , the Middle and North Fork drainages of the John Day River , and the peaks of the Strawberry Mountain Wilderness to the south. Many species of alpine wildflower found west of the Rocky Mountains grow in the area. Big game species and upland game birds are common. The area's rich geologic past means
108-430: Is currently an elk herd estimated to number beyond 50,000 and a herd of mule deer that reportedly exceeds 150,000. Bull elk here sometimes weigh more than 800 pounds (360 kg) and sport antlers spreading beyond 5 feet (1.5 m). There are over 130 miles (210 km) of perennial streams in the wilderness, 40 miles (64 km) of which provide spawning habitat for chinook salmon and steelhead . Other wildlife in
126-406: The Vinegar Hill-Indian Rock Scenic Area also lie within the wilderness. The North Fork John Day Wilderness is located within the larger Elkhorn Fire Management Area, and the area's fire plan allows for the use of Prescribed Natural Fire under certain circumstances. The North Fork John Day Wilderness is composed of rolling benchlands, steep ridges, alpine lake basins, and the granite outcrops of
144-563: The Wilderness Act 's purpose to have no permanent human works in wilderness areas. The Sumpter Valley Gold Dredge once excavated the riverbeds in the area, and is now restored as a state heritage site in Sumpter . The North Fork John Day Wilderness is known for its big game and anadromous fish habitat. Dominant wildlife species include Rocky Mountain elk and mule deer . There is currently an elk herd estimated to number beyond 50,000 and
162-585: The granite cores of the Elkhorn and Greenhorn ranges. Columbia River basalt flows buried the region some 15 million years ago, the remains of which can be seen today in the rimrock on the benchlands in the western portion of the wilderness. The North Fork John Day drainage bustled with gold and silver mining operations in the mid-19th century, and traces of the thousands of miners who labored here are still visible. Old mining structures, building foundations, and dredged ditches and trash dumps left behind by
180-560: The Greenhorn Mountains at an elevation of 8,100 feet (2,500 m). It encompasses two entire subranges of the Blue Mountains—the Greenhorn Mountains and the ragged Elkhorn Mountains. A continuous vegetative canopy covers most of the land, including dense virgin stands of conifer species like Douglas-fir , white fir , western larch and lodgepole pine . The headwaters of several waterways are located in
198-609: The North Fork John Day Wilderness include mountain goats and black bears . Primary recreational activities in the North Fork John Day Wilderness are hiking, camping, horseback riding, hunting, fishing, cross-country skiing, rafting, kayaking, wildlife watching, and rock climbing the granite cliffs of the Elkhorn Mountains. There are roughly 133 miles (214 km) of hiking trails in the wilderness, three of which are National Recreation Trails . Vinegar Hill-Indian Rock Scenic Area The Vinegar Hill-Indian Rock Scenic Area
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#1732858128147216-514: The North Fork John Day Wilderness reflect the Blue Mountains' history as a volcanic island archipelago in the Pacific Ocean some 250 million years ago. As the crust of the earth shifted, the archipelago collided with the advancing North American Plate approximately 200 million years ago. Later, bubbles of less dense granitic rock, or batholiths , rose through the sediment to form
234-414: The crust of the earth shifted, the archipelago collided with the advancing North American Plate approximately 200 million years ago. Later, bubbles of less dense granitic rock, or batholiths , rose through the sediment to form the granite cores of the Elkhorn and Greenhorn ranges. Columbia River basalt flows buried the region some 15 million years ago, the remains of which can be seen today in
252-431: The larger Elkhorn Fire Management Area, and the area's fire plan allows for the use of Prescribed Natural Fire under certain circumstances. The North Fork John Day Wilderness is composed of rolling benchlands, steep ridges, alpine lake basins, and the granite outcrops of the Greenhorn Mountains at an elevation of 8,100 feet (2,500 m). It encompasses two entire subranges of the Blue Mountains—the Greenhorn Mountains and
270-517: The miners are all visible. Many of these features are being left in place to naturally disappear over time, consistent with the Wilderness Act 's purpose to have no permanent human works in wilderness areas. The Sumpter Valley Gold Dredge once excavated the riverbeds in the area, and is now restored as a state heritage site in Sumpter . The North Fork John Day Wilderness is known for its big game and anadromous fish habitat. Dominant wildlife species include Rocky Mountain elk and mule deer . There
288-562: The ragged Elkhorn Mountains. A continuous vegetative canopy covers most of the land, including dense virgin stands of conifer species like Douglas-fir , white fir , western larch and lodgepole pine . The headwaters of several waterways are located in the wilderness, including Bull Creek, Baldy Creek, and Crawfish Creek, as well as the North Fork John Day River , 39 miles (63 km) of which are designated Wild and Scenic . The granite and sedimentary rock that makes up much of
306-484: The rimrock on the benchlands in the western portion of the wilderness. The North Fork John Day drainage bustled with gold and silver mining operations in the mid-19th century, and traces of the thousands of miners who labored here are still visible. Old mining structures, building foundations, and dredged ditches and trash dumps left behind by the miners are all visible. Many of these features are being left in place to naturally disappear over time, consistent with
324-404: The wilderness, including Bull Creek, Baldy Creek, and Crawfish Creek, as well as the North Fork John Day River , 39 miles (63 km) of which are designated Wild and Scenic . The granite and sedimentary rock that makes up much of the North Fork John Day Wilderness reflect the Blue Mountains' history as a volcanic island archipelago in the Pacific Ocean some 250 million years ago. As
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