http://maps.google.com/?ie=UTF8&ll=45.2 ... 4&t=p&z=15
http://www.mthood.info/hikingtrails/salmonriver742.pdf
http://www.go-oregon.net/Linney-Creek-Trail-499-Oregon
http://www.fs.fed.us/r6/mthood/projects ... lt3mod.pdf
The Salmon River rises on the south slope of Mount Hood, fed by the melting ice of the Palmer Glacier. From its alpine beginnings, the river flows swiftly south down the flank of the volcano, carving a maze of steep canyons in the soft pumice and ash that makes up the smooth south slopes of Mount Hood. At the southern base of the mountain, the river slows as it meanders through lush alpine meadows, first through marshy Red Top Meadows, and then the sprawling Salmon River Meadows. From here, Mount Hood towers above the stream, the meadows having formed over the centuries where a massive, ancient pyroclastic flow buried this part of the Salmon River canyon with hundreds of feet of volcanic debris. The meadows of today are where the river meandered across the flat surface of the debris.Soon, the Salmon River enters deep forest at the south edge of the meadows, and turns west, as it enters the Salmon River Gorge. At first, the river rambles through the upper gorge, rushing over boulders, and picking up tributaries along the way. Then, at Linney Creek, the gorge suddenly deepens. The river plunges into a steep, spectacular canyon, with black basalt cliffs rising hundreds of feet above the stream. Here, the Salmon River enters the Salmon-Huckleberry Wilderness, and roars over six named waterfalls, and several unnamed cataracts as it flows over the ancient bedrock of the Old Cascades. The forest becomes rainforest here, with sheer cliffs coated in thick green mats of moss and ferns, and massive old growth conifers soaring above the stream.Below the gorge, the river becomes wider, with sweeping bends and deep pools where the stream rushes over wide gravel bars and slides over smooth bedrock. Here, the ancient forest spreads out, with lush woodlands sweeping up from the river into the surrounding mountains. At the junction with the South Fork, the river leaves the Salmon-Huckleberry Wilderness, and rambles past forest campgrounds and summer cabins before joining the Sandy River, another glacial stream that originates on Mount Hood.The Salmon was designated a National Wild and Scenic River in 1988, and is home to endangered Steelhead and Chinook salmon. The river offers one of the few spawning habitats in the Columbia basin that is unimpeded by dams, and special restrictions on fishing are in place here, as a result. The Salmon River rises on the south slope of Mount Hood, fed by the melting ice of the Palmer Glacier. From its alpine beginnings, the river flows swiftly south down the flank of the volcano, carving a maze of steep canyons in the soft pumice and ash that makes up the smooth south slopes of Mount Hood. At the southern base of the mountain, the river slows as it meanders through lush alpine meadows, first through marshy Red Top Meadows, and then the sprawling Salmon River Meadows. From here, Mount Hood towers above the stream, the meadows having formed over the centuries where a massive, ancient pyroclastic flow buried this part of the Salmon River canyon with hundreds of feet of volcanic debris. The meadows of today are where the river meandered across the flat surface of the debris.Soon, the Salmon River enters deep forest at the south edge of the meadows, and turns west, as it enters the Salmon River Gorge. At first, the river rambles through the upper gorge, rushing over boulders, and picking up tributaries along the way. Then, at Linney Creek, the gorge suddenly deepens. The river plunges into a steep, spectacular canyon, with black basalt cliffs rising hundreds of feet above the stream. Here, the Salmon River enters the Salmon-Huckleberry Wilderness, and roars over six named waterfalls, and several unnamed cataracts as it flows over the ancient bedrock of the Old Cascades. The forest becomes rainforest here, with sheer cliffs coated in thick green mats of moss and ferns, and massive old growth conifers soaring above the stream.Below the gorge, the river becomes wider, with sweeping bends and deep pools where the stream rushes over wide gravel bars and slides over smooth bedrock. Here, the ancient forest spreads out, with lush woodlands sweeping up from the river into the surrounding mountains. At the junction with the South Fork, the river leaves the Salmon-Huckleberry Wilderness, and rambles past forest campgrounds and summer cabins before joining the Sandy River, another glacial stream that originates on Mount Hood.The Salmon was designated a National Wild and Scenic River in 1988, and is home to endangered Steelhead and Chinook salmon. The river offers one of the few spawning habitats in the Columbia basin that is unimpeded by dams, and special restrictions on fishing are in place here, as a result.
