query: where is the cascade range located on a map

pos: Cascade Range Cascade Range The Cascade Range or Cascades is a major mountain range of western North America, extending from southern British Columbia through Washington and Oregon to Northern California. It includes both non-volcanic mountains, such as the North Cascades, and the notable volcanoes known as the High Cascades. The small part of the range in British Columbia is referred to as the Canadian Cascades or, locally, as the Cascade Mountains. The latter term is also sometimes used by Washington residents to refer to the Washington section of the Cascades in addition to North Cascades, the more usual U.S. term, as in

pos: Chutla Peak Chutla Peak Chutla Peak is a summit on the crest of the Tatoosh Range which is a sub-range of the Cascade Range. It's located south of Mount Rainier within Mount Rainier National Park. The mountain's name "Chutla" derives from Chinook Jargon which means "rock". Precipitation runoff on the peak drains into the Nisqually River. Chutla Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift),

pos: Mount Teneriffe (Washington) Mount Teneriffe (Washington) Mount Teneriffe is a mountain located in King County of Washington state. The mountain is 1,459 meters high and is located at the western edge of the Cascade Range on land managed by Mount Baker-Snoqualmie National Forest. The mountain takes its name from the island of Tenerife in Spain. Mount Teneriffe is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop

pos: Alta Mountain Wilderness area. Alta Mountain Alta Mountain is a mountain summit located in Kittitas County in Washington state. It is within the Alpine Lakes Wilderness which is part of the Cascade Range. Alta Mountain is situated on land managed by Mount Baker-Snoqualmie National Forest. Precipitation runoff from the mountain drains into tributaries of the Yakima River. Alta Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing

pos: Alta Mountain Alta Mountain Alta Mountain is a mountain summit located in Kittitas County in Washington state. It is within the Alpine Lakes Wilderness which is part of the Cascade Range. Alta Mountain is situated on land managed by Mount Baker-Snoqualmie National Forest. Precipitation runoff from the mountain drains into tributaries of the Yakima River. Alta Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to

pos: Tower Mountain (Washington) Tower Mountain (Washington) Tower Mountain is a prominent non-volcanic mountain located on the boundary line of Okanogan and Skagit counties in Washington state. It is part of the Okanogan Range which is a sub-range of the North Cascades Range. Tower Mountain situated on land administered by Okanogan National Forest. Tower Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop

pos: The Needles (Washington) The Needles (Washington) The Needles is a granite mountain located in Okanogan County in Washington state. It is part of the Okanogan Range which is a sub-range of the North Cascades Range. The Needles is situated on land administered by Okanogan National Forest. The nearest higher peak is Tower Mountain, to the southwest. The Needles is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range,

pos: Chutla Peak influence, snow tends to be wet and heavy, resulting in high avalanche danger. Chutla Peak Chutla Peak is a summit on the crest of the Tatoosh Range which is a sub-range of the Cascade Range. It's located south of Mount Rainier within Mount Rainier National Park. The mountain's name "Chutla" derives from Chinook Jargon which means "rock". Precipitation runoff on the peak drains into the Nisqually River. Chutla Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach,

pos: Stevens Peak Stevens Peak Stevens Peak is a summit in the Tatoosh Range which is a sub-range of the Cascade Range. It's located in Mount Rainier National Park, one mile east of Unicorn Peak. The name honors Hazard Stevens who made the first documented ascent of Mount Rainier along with P. B. Van Trump on August 17, 1870. Precipitation runoff from the mountain drains into tributaries of the Cowlitz River. Stevens Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts

pos: Big Kangaroo Big Kangaroo Big Kangaroo is a granitic mountain located in Okanogan County, Washington. The mountain is part of the Methow Mountains in the Cascade Range. Big Kangaroo is the high point of Kangaroo Ridge which is about two miles east and within view of Washington Pass. Big Kangaroo is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in

pos: Double Peak (Washington) Double Peak (Washington) Double Peak is the descriptive name of a double summit located in Mount Rainier National Park in Pierce County of Washington state. Part of the Cascade Range, it is situated northwest of Shriner Peak, south of Governors Ridge, and southeast of the Cowlitz Chimneys. Double Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in

pos: The Triplets (Washington) The Triplets (Washington) The Triplets is a summit located in Skagit County of Washington state. This breccia triple pinnacle is part of the North Cascades Range. The Triplets is situated above Cascade Pass on the shared border of North Cascades National Park and Glacier Peak Wilderness. The nearest higher peak is Cascade Peak to the west-northwest. Surface runoff from the mountain drains into the Cascade River (Washington). The Triplets is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach

pos: Unicorn Peak Unicorn Peak Unicorn Peak is the highest point in the Tatoosh Range which is a sub-range of the Cascade Range. It's located in Mount Rainier National Park, south of Mount Rainier. The descriptive name is for the mountain's resemblance to the head and horn of a unicorn. Precipitation runoff from the mountain's small glaciers, such as Unicorn Glacier, drains into tributaries of the Cowlitz River. Unicorn Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are

pos: West Unicorn Peak West Unicorn Peak West Unicorn Peak is the second highest point in the Tatoosh Range which is a sub-range of the Cascade Range. It is located south of Mount Rainier within Mount Rainier National Park, in Lewis County of Washington state. The nearest higher peak is Unicorn Peak, to the east-northeast. Precipitation runoff and meltwater from the peak's small glacier, Unicorn Glacier, drain into tributaries of the Cowlitz River. West Unicorn Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains.

pos: McClellan Butte McClellan Butte McClellan Butte is a prominent peak in the Cascade Range in King County, Washington 11 miles east of North Bend. The McClellan Butte hiking trail is a difficult trail known as an alternative to Mount Si's crowded trail. McClellan Butte is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades

pos: Preacher Mountain Preacher Mountain Preacher Mountain is a broad summit located in King County of Washington state. It's located at the western edge of the Cascade Range and is within the Alpine Lakes Wilderness on land managed by Mount Baker-Snoqualmie National Forest. The nearest higher peak is Kaleetan Peak, to the southeast. The Pulpit is situated 2.19 miles to the northwest. Precipitation runoff from the mountain drains into tributaries of the Snoqualmie River. Preacher Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade

pos: Bandera Mountain Bandera Mountain Bandera Mountain is a mountain located near Snoqualmie Pass, Washington in the Alpine Lakes Wilderness.The mountain is accessible by the Mason Lake Trail (Ira Springs Memorial Trail), which is located off I-90 at Exit 45 on Forest Road 9031. Bandera Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the

pos: Tatoosh Peak Tatoosh Peak Tatoosh Peak is a summit in the Tatoosh Range which is a sub-range of the Cascade Range. It's the highest point in the Tatoosh Wilderness, a protected area which is managed by Gifford Pinchot National Forest. The name "tatoosh" derives from Chinook Jargon which means "breast". Precipitation runoff from the peak drains into tributaries of the Cowlitz River. Tatoosh Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks

pos: Beebe Mountain Beebe Mountain Beebe Mountain is a summit in the Cascade Range in the U.S. state of Washington. It is located on the border of North Cascades National Park. The mountain's name honors Frank Beebe who worked for the Forest Service and maintained a cabin near the base of the mountain in the 1920s. Precipitation runoff on the mountain drains into Ross Lake via Granite Creek and Panther Creek. Beebe Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts

pos: Trapper Mountain Trapper Mountain Trapper Mountain is a summit located in Chelan County of Washington state. It is part of the North Cascades Range. Trapper Mountain is situated southeast of Cascade Pass on the shared border of North Cascades National Park and Glacier Peak Wilderness. The nearest higher peak is Hurry-up Peak, to the west. Surface runoff from the mountain drains into Trapper Lake and tributaries of the Stehekin River. Trapper Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts

pos: Pinnacle Peak (King County, Washington) built on the summit was called the Pinnacle Peak Lookout, hence the name "Pinnacle Peak" emerged. The one mile trail on the north side of Pinnacle Peak is called the "Cal Magnusson Trail" for a long time Cascade mountaineer who worked at REI for 25 years with famed American mountain climber Jim Whittaker. Pinnacle Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to

pos: Denny Mountain Denny Mountain Denny Mountain is summit near Snoqualmie Pass in Washington state. The Alpental ski area is located on the mountain's eastern flank. The mountain is named after Arthur A. Denny of the Denny Party, who oversaw the construction of the Snoqualmie Pass Road, which later became I-90, and which runs along the mountain's southern base. Denny Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range,

pos: Fisher Peak (Washington) Fisher Peak (Washington) Fisher Peak is a summit in the Cascade Range in the U.S. state of Washington. It is located on the borders of the Stephen Mather Wilderness and North Cascades National Park. It's situated midway between Black Peak and Easy Pass, adjacent to Repulse Peak. Precipitation runoff from Fisher Peak drains into tributaries of the Skagit River. Fisher Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by

pos: Holliway Mountain Holliway Mountain Holliway Mountain is an 8000+ ft granite summit located in Okanogan County in Washington state. It is part of the Okanogan Range which is a sub-range of the North Cascades Range. Holliway Mountain is situated near the headwaters of the Methow River on land administered by Okanogan National Forest. The nearest higher peak is Golden Horn, to the south. Azurite Peak is located three miles to the north-northwest. Holliway Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains.

pos: Lane Peak Lane Peak Lane Peak is a summit on the crest of the Tatoosh Range which is a sub-range of the Cascade Range. It's located south of Mount Rainier within Mount Rainier National Park. Lane Peak honors United States Secretary of the Interior Franklin Knight Lane who presided over the establishment of the National Park Service in 1917. Precipitation runoff on the south side of the peak drains into tributaries of the Cowlitz River, whereas the north side drains into tributaries of the Nisqually River. Lane Peak is located in the marine west coast climate zone of western North America. Most

pos: Hurry-up Peak S Glacier rests on the eastern flank of the peak and meltwater from it drains into Trapper Lake. Precipitation runoff on the east side the mountain drains into tributaries of the Stehekin River, while precipitation drains into the Cascade River from the west side. Hurry-up Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form

pos: Mix-up Peak eastern flank. Surface runoff on the east side the mountain drains into the Stehekin River, whereas precipitation runoff drains into the Cascade River from the west side. Mix-up Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the

pos: Golden Horn (Washington) Golden Horn (Washington) Golden Horn is a granite mountain located in Okanogan County in Washington state. It is part of the Okanogan Range which is a sub-range of the North Cascades Range. Golden Horn is situated north of Methow Pass at headwaters of the Methow River on land administered by Okanogan National Forest. The nearest higher peak is Tower Mountain, to the southeast. Golden Horn is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they

pos: Wahpenayo Peak Wahpenayo Peak Wahpenayo Peak is a 6,231 ft summit in the Tatoosh Range which is a sub-range of the Cascade Range. It is located south of Mount Rainier within Mount Rainier National Park, in Lewis County of Washington state. The mountain is named for "Wahpenayo", a native American chief who was the father-in-law of Indian Henry. Precipitation runoff on the south and east side of the peak drains into tributaries of the Cowlitz River, whereas the north side drains into tributaries of the Nisqually River. Wahpenayo Peak is located in the marine west coast climate zone of western North America.

pos: Gunn Peak Gunn Peak Gunn Peak is a mountain located in Snohomish County, Washington. The mountain is part of the Cascade Range. Gunn Peak is the highest point of the Wild Sky Wilderness. The mountain was named for homesteader/miner Amos Gunn who started the nearby town of Index, Washington, and also named nearby Mount Index. Precipitation runoff from the mountain drains into tributaries of the Skykomish River Gunn Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North

pos: Mount Dickerman Mount Dickerman Mount Dickerman, or Dickerman Mountain, is a mountain in Mount Baker-Snoqualmie National Forest in Washington state. It is located northwest of Barlow Pass along the Mountain Loop Highway]. A strenuous four mile trail leads from this highway to the summit with views which includes Glacier Peak, Monte Cristo Peak, and Sloan Peak. Dickerman is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range,

pos: Barrier Peak Barrier Peak Barrier Peak is a small 6,521 ft (1,988 m) summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Cascade Range and is situated west of Cayuse Pass, 0.53 mile west-northwest of Buell Peak, and 0.4 mile south-southwest of Governors Ridge, which is its nearest higher peak. The normal climbing access is from the Owyhigh Lakes Trail. Barrier Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach,

pos: Cache Col col drains into the Stehekin River, while precipitation drains into the Cascade River from the south side. Cache Col is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months

pos: Magic Mountain (Washington) into the Cascade River from the southwest side. Magic Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather

neg: White Pass Ski Area second high-speed detachable quad. The expansion required a new trail map to show the new terrain. The new map was drawn by James Niehues and will be redrawn for the 2011–12 season to show runs that are not on the current trail map. Many runs also still need to be named because White Pass Ski Area wanted to let everyone ski on the expansion, then decide the names of the runs via Facebook. White Pass Ski Area The White Pass Ski Area is a ski area in the northwest United States, in the Cascade Range at White Pass, Washington. Located

neg: Cascade Pass first white men to explore and map the Skagit Pass was New York newspaperman Frank Wilkeson. Alexander Ross probably crossed the Cascades via Cascade Pass in 1814. His writings are too vague to be certain about his precise route. Cascade Pass Cascade Pass (formerly also known as Skagit Pass) is a mountain pass over the northern Cascade Range, east of Marblemount, Washington, U.S. Although an important pass, providing the easiest connection from the Cascade River to the head of Lake Chelan, it is now inside North Cascades National Park, and crossed by only a hiking trail. From the west, one

neg: Yamsay Mountain Mount Bachelor, Mount Shasta, the Three Sisters, and Mount Thielsen. Other activities along the trail include hiking and horseback riding up the mountain from the recreation area located at an elevation between . Yamsay Mountain Yamsay Mountain is a large shield volcano in the Cascade Range of south-central Oregon, located about east of Crater Lake on the border between Klamath County and Lake County. It is part of the Cascade Volcanic Arc but is located in a mountain range behind the main Cascade volcanic front. The best known members of this enigmatic arc are the massive shields of Newberry Volcano,

neg: Horse Rock Ridge Concern (ACEC). Elevations within the RNA vary from to . A hiking trail on Horse Rock Ridge includes views of the Three Sisters, Mount Jefferson and other Cascade peaks. Horse Rock Ridge Horse Rock Ridge is a ridgetop located on the western edge of the Cascade Range near Crawfordsville, Oregon. The site is recognized for its considerable diversity of plant species that includes both Willamette Valley plants as well as plants more often found in the mountain zone of the Cascade Range. There are also several plant species more often found east of the Cascade Range. The Horse Rock Ridge

neg: Yamsay Mountain Yamsay Mountain Yamsay Mountain is a large shield volcano in the Cascade Range of south-central Oregon, located about east of Crater Lake on the border between Klamath County and Lake County. It is part of the Cascade Volcanic Arc but is located in a mountain range behind the main Cascade volcanic front. The best known members of this enigmatic arc are the massive shields of Newberry Volcano, about farther north in Oregon, and Medicine Lake Volcano, about south in Northern California. Yamsay is the highest volcano in the eastern arc, almost higher than Newberry and Medicine Lake. A central part

neg: Vancouver, Washington Vancouver would have passed Tacoma and Spokane to become the state's second-largest city. Vancouver is located just north of the Columbia River, just west of where the Columbia River Gorge bisects the volcanic Cascade Range and just east of where the Willamette River enters the Columbia. The city of Vancouver is in the Western Lowlands region of Washington. When clouds do not blanket the Puget-Willamette trough formed by the Cascade and Coast Range, Mount Hood, Mount Saint Helens, Mount Jefferson and Mount Adams are all visible from Vancouver. According to the United States Census Bureau, the city has a total

neg: Horse Rock Ridge Horse Rock Ridge Horse Rock Ridge is a ridgetop located on the western edge of the Cascade Range near Crawfordsville, Oregon. The site is recognized for its considerable diversity of plant species that includes both Willamette Valley plants as well as plants more often found in the mountain zone of the Cascade Range. There are also several plant species more often found east of the Cascade Range. The Horse Rock Ridge Research Natural Area (RNA) is managed by the Bureau of Land Management (BLM). It is designated by the BLM as both an RNA and an Area of Critical Environmental

neg: Sierra Nevada (U.S.) the southern extent of Cenozoic igneous surface rock from the Cascade Range. It is bounded on the west by California's Central Valley and on the east by the Basin and Range Province. The southern boundary is at Tehachapi Pass. Physiographically, the Sierra is a section of the Cascade-Sierra Mountains province, which in turn is part of the larger Pacific Mountain System physiographic division. The California Geological Survey states that "the northern Sierra boundary is marked where bedrock disappears under the Cenozoic volcanic cover of the Cascade Range." The range is drained on its western slope by the Central Valley watershed,

neg: Cascade Peaks Cascade Peaks The Cascade Peaks are three summits in the Monte Perdido Range of the Pyrenees, culminating at on the eastern peak. The central peak, known as Brulle, and the western peak are and high, respectively. The peaks are located on the 3,000 m French-Spanish borderline crest. The central summit was named in honor of Henri Brulle. The peaks are part of the Monte Perdido Range above the Cirque de Gavarnie. The peaks are located in the Hautes-Pyrénées department, in the Midi-Pyrénées region of France, and in Huesca province, in the Aragon region of Spain. The summit is composed of

neg: Lassen Peak southern entrance to the park area has a winter sports area where visitors can ski, and within the Lassen National Forest, visitors can also bicycle, go boating, or use snowmobiles. Lassen Peak Lassen Peak, commonly referred to as Mount Lassen, is the southernmost active volcano in the Cascade Range of the Western United States. Located in the Shasta Cascade region of Northern California, it is part of the Cascade Volcanic Arc, which stretches from southwestern British Columbia to northern California. Lassen Peak reaches an elevation of , standing above the northern Sacramento Valley. It supports many flora and fauna among

neg: Mount Mazama magnesium and iron) andesite to the west and southwest, with high-volume rhyodacite lava flows from 600,000 to 700,000 years old underlying Mazama deposits to the south, southeast, east, and northeast. It is a major Cascade volcano, and is located at the intersection of the Cascade Range and Klamath graben, the north–northwest trending basin also surrounded by fault zones. The Basin and Range Province lies to the east. Mazama lies within the broad segment of the Cascades arc, where smaller volcanoes are common because of melting patterns of the Earth's mantle within the region. Erupting magma that ranged from high-alumina olivine

neg: The Pulpit (Washington) processes which have created the tall peaks and deep valleys of the Cascade Range. The Pulpit (Washington) The Pulpit is a mountain summit located in King County of Washington state. It's located at the western edge of the Cascade Range on land managed by Mount Baker-Snoqualmie National Forest. The Pulpit is more notable for its large, steep rise above local terrain than for its absolute elevation. The nearest higher peak is Preacher Mountain, to the southeast. Precipitation runoff from The Pulpit drains into tributaries of the Snoqualmie River. The Pulpit is located in the marine west coast climate zone of

neg: Little Comrade (Washington) processes which have created the tall peaks and deep valleys of the Cascade Range. Little Comrade (Washington) Little Comrade is a small summit located in King County of Washington state. It's located at the western edge of the Cascade Range on land managed by Mount Baker-Snoqualmie National Forest. Little Comrade is more notable for its large, steep rise above local terrain than for its absolute elevation. The nearest higher peak is Russian Butte, to the north-northeast. Precipitation runoff from Little Comrade drains into tributaries of the Snoqualmie River. Little Comrade is located in the marine west coast climate zone of

neg: Jabberwocky Tower Jabberwocky Tower Jabberwocky Tower is a 6,480 ft granite spire located in Chelan County of Washington state. Jabberwocky Tower is part of The Enchantments within the Alpine Lakes Wilderness. It belongs to the Stuart Range which is subset of the Cascade Range. Jabberwocky Tower is situated east of Colchuck Lake and west of Enchantment Peak. Precipitation runoff drains into Icicle Creek, a tributary of the Wenatchee River. Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop

neg: Broken Top Broken Top Broken Top is a glacially eroded complex stratovolcano. It lies in the Cascade Volcanic Arc, part of the extensive Cascade Range in the U.S. state of Oregon. Located southeast of the Three Sisters peaks, the volcano, residing within the Three Sisters Wilderness, is west of Bend, Oregon in Deschutes County. Eruptive activity stopped roughly 100,000 years ago, and currently, erosion by glaciers has reduced the volcano's cone to where its contents are exposed. There are two named glaciers on the peak, Bend and Crook Glacier. Diverse species of flora and fauna inhabit the area, which is subject to

neg: Cascade Peaks massive algae sediments, miliolitic sediments (eolianite) and sandstone sediments from the Eocene and Oligocene periods. Cascade Peaks The Cascade Peaks are three summits in the Monte Perdido Range of the Pyrenees, culminating at on the eastern peak. The central peak, known as Brulle, and the western peak are and high, respectively. The peaks are located on the 3,000 m French-Spanish borderline crest. The central summit was named in honor of Henri Brulle. The peaks are part of the Monte Perdido Range above the Cirque de Gavarnie. The peaks are located in the Hautes-Pyrénées department, in the Midi-Pyrénées region of France,

neg: Russian Butte of that recent glaciation. Uplift and faulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the Cascade Range. Russian Butte Russian Butte is a double-peak summit located in King County of Washington state. It's located at the western edge of the Cascade Range on land managed by Mount Baker-Snoqualmie National Forest. Russian Butte is more notable for its large, steep rise above local terrain than for its absolute elevation. The nearest higher officially named peak is Preacher Mountain, to the east. Little Comrade is a small peak 0.5 mile

neg: Washington wine planted as of 2008. Similar to the Columbia Valley and Walla Walla AVAs, this appellation also crosses over the southern Washington border into Oregon where Pinot noir and Pinot gris are grown. Located along the Columbia River where it bisects the Cascade Range, parts of the AVA fall within a wind tunnel that is a popular tourist destination for wind surfing but can be too fierce for viticulture. Most of the vineyards planted on the Washington side of the appellation are located on southward facing slopes along the river where they can receive some protection from the winds. Depending upon

neg: Stellar pulsation shows a period doubling bifurcation, or cascade, leading to chaos. The near quadratic shape of the map is indicative of chaos and implies an underlying horseshoe map. Other sequences of models follow a somewhat different route, but also to chaos, namely the Pommeau-Manneville or "tangent bifurcation" route. The following shows a similar visualization of the period doubling cascade to chaos for a sequence of stellar models that differ by their average surface temperature T. The graph shows triplets of values of the stellar radius (R, R, R) where the indices , indicate successive time intervals. The presence of low dimensional

neg: Shasta Cascade Lake, Lassen Volcanic National Park, Caribou Wilderness, Thousand Lakes Wilderness, and climbing Mount Shasta. The civic "capital" of the Shasta Cascade area is Redding; other cities and towns are Alturas, Biggs, Chico, Dunsmuir, Mount Shasta, Red Bluff, Oroville, Paradise, Weed, Fall River Mills, Burney, and Yreka. Counties included in the Shasta Cascade region include Butte, Lassen, Modoc, Plumas, Shasta, Siskiyou, Tehama and Trinity. Geologically, this region is similar to the main Cascade Range, dominated by volcanism. Shasta Cascade The Shasta Cascade region of California is located in the northeastern and north-central sections of the state bordering Oregon and Nevada, including

neg: Mount Pilchuck of the Cascade range to the east, and the Puget Sound to the west. At Mount Pilchuck's summit is an old fire lookout, now used as shelter for hikers. This former lookout is jointly maintained by Washington State Parks and the Everett branch of The Mountaineers. Some years the trail to the summit is still covered with snow until late in the summer. Mount Pilchuck Mount Pilchuck is a mountain located in Snohomish County, Washington. It is northeast of Seattle. It is part of the Cascade Range. Mount Pilchuck is located within Mount Pilchuck State Park, but the area surrounding

neg: Pilot Rock (Oregon) in elevation. At the summit, there are views of landmarks such as Mount Shasta, the Trinity Alps, and Mount McLoughlin. Pilot Rock (Oregon) Pilot Rock is a prominent volcanic plug located in the western Cascade Range near the east end of the Siskiyou Mountains, just east of the Siskiyou Summit near Ashland, Oregon. Rising thousands of feet above the Shasta and Rogue valleys, it is a landmark distinguishable from over away. At 25.6 million years old, it is one of the oldest formations of the Cascade Range. The rock is protected by the Cascade–Siskiyou National Monument and the Soda Mountain

neg: Pilot Rock (Oregon) Pilot Rock (Oregon) Pilot Rock is a prominent volcanic plug located in the western Cascade Range near the east end of the Siskiyou Mountains, just east of the Siskiyou Summit near Ashland, Oregon. Rising thousands of feet above the Shasta and Rogue valleys, it is a landmark distinguishable from over away. At 25.6 million years old, it is one of the oldest formations of the Cascade Range. The rock is protected by the Cascade–Siskiyou National Monument and the Soda Mountain Wilderness. Several trails pass near Pilot Rock, including the Pacific Crest Trail. Rising above the surrounding hills and thousands of

neg: Hall J. Kelley of the British Hudson's Bay Company, which actively discouraged U.S. settlement. Kelley wrote articles to encourage U.S. settlers to move into Oregon Country. This included a memorial to the United States Congress on February 11, 1828, that laid out plans for a city where the Columbia River meets the Willamette River (present-day Portland, Oregon) and a proposal to name mountains in the Cascade Range after US presidents. In 1830, he published a "Geographical Memoir of Oregon", which contained the first map of that territory ever compiled, as well as a settlement guide for prospective emigrants. Kelley's writings were influential in

neg: Little Cultus Lake Little Cultus Lake Little Cultus Lake is a natural lake in Deschutes County, Oregon, United States. Near its larger and more popular twin Cultus Lake to the north on the other side of Cultus Mountain, it is located in the Deschutes National Forest in the Cascade Range. Like Cultus Lake, it is named after the Chinook Jargon word "cultus", meaning "in vain" or "worthless". Little Cultus Lake is located a little more than directly south of Cultus Lake, and southwest of Bend. It is located off of the Cascade Lakes Scenic Byway, which winds through the terrain featuring similar natural

neg: Cascade Volcanoes the subduction zone. At issue are the current estimates of plate configuration and rate of subduction, but based on the chemistry of these volcanoes, they are also subduction related and therefore part of the Cascade Volcanic Arc. The Cascade Volcanic Arc appears to be segmented; the central portion of the arc is the most active and the northern end least active. Lavas representing the earliest stage in the development of the Cascade Volcanic Arc mostly crop out south of the North Cascades proper, where uplift of the Cascade Range has been less, and a thicker blanket of Cascade Arc volcanic

neg: Culp Creek, Oregon Culp Creek, Oregon Culp Creek is an unincorporated community in Lane County, Oregon, United States, southeast of Cottage Grove on the Row River. It lies on Row River Road between Dorena and Disston. This populated place is located above sea level in the foothills of the Cascade Range. The community is located where the Row River receives the stream that shares its name with the community. Hawley Butte lies just north of Culp Creek and stands tall. Culp Creek is a tributary stream of the Row River, and was named for settler John Culp just before 1900. A logging camp

neg: Plumas County, California Plumas County is located in the far northern end of the Sierra Nevada range. The area's rugged terrain marks the transition point between the northern Sierra Nevadas and the southern end of the Cascade Range. Lassen Peak, which is the southernmost volcanic peak in the Cascade Range, is found just north of Plumas County's border, and part of Lassen Volcanic National Park extends into the northwest corner of the county. Plumas National Forest's offer a wide variety of outdoor recreation opportunities, including hiking, camping, kayaking, swimming, mountain biking, hunting and fishing. The area features more than 100 natural and artificial

neg: Mount Baker older than 80–90,000 years. Older volcanic edifices have mostly eroded away due to glaciation. After Mount Rainier, Mount Baker is the most heavily glaciated of the Cascade Range volcanoes; the volume of snow and ice on Mount Baker, is greater than that of all the other Cascades volcanoes (except Rainier) combined. It is also one of the snowiest places in the world; in 1999, Mount Baker Ski Area, located to the northeast, set the world record for recorded snowfall in a single season—. At , it is the third-highest mountain in Washington and the fifth-highest in the Cascade Range, if

neg: Elk Lake Guard Station The Elk Lake Guard Station is listed on the National Register of Historic Places. Elk Lake Guard Station is located in the eastern foothills of the Cascade Range in central Oregon. It is southwest of Bend. The guard station is just off Forest Road 46, also known as the Cascade Lakes National Scenic Byway. The compound is situated between the east side of the highway and the northwest shore of the Elk Lake. The site is at an elevation of above sea level. The area around the guard station is a coniferous forest dominated by lodgepole pine. The Cascade Lakes

neg: Lassen Peak Lassen Peak Lassen Peak, commonly referred to as Mount Lassen, is the southernmost active volcano in the Cascade Range of the Western United States. Located in the Shasta Cascade region of Northern California, it is part of the Cascade Volcanic Arc, which stretches from southwestern British Columbia to northern California. Lassen Peak reaches an elevation of , standing above the northern Sacramento Valley. It supports many flora and fauna among its diverse habitats, which are subject to frequent snowfall and reach high elevations. A lava dome, Lassen Peak has a volume of making it the largest lava dome on Earth.

neg: Calapooya Mountains Mountains and the Calapooya Divide are two parts of a spur of the Western Cascade mountains in the U.S. state of Oregon that form the divide between the watersheds of the Willamette and Umpqua rivers. At its southeastern end, the spur joins the Cascade Range near Cowhorn Mountain near the headwaters of the Middle Fork Willamette River and the North Umpqua River. A topographic map in the "Atlas of Oregon" shows the Calapooya Mountains curving northwest from near Potter, McGowan, and Balm mountains past Bohemia Mountain to Holland Point, south of Oakridge. From near Bohemia Mountain, a block of mountains

neg: Ocooch Mountains and rugged, supporting a heavy growth of pine, &c. while the latter often present extensive flats, abounding in lakes, swamps, and ponds, yielding wild rice in great abundance and perfection." Keating's report on the 1823 Long expedition included a "Map of the country embracing the route of the expedition of 1823 commanded by Major S.H. Long". The name Ocooch is placed on this map approximately where the Baraboo Hills are located. Hachures extend the range to the north and northwest, but the implication is that the name Ocooch applied only to its southernmost end. An 1833 map, "Northwest and Michigan

neg: Shasta Cascade Shasta Cascade The Shasta Cascade region of California is located in the northeastern and north-central sections of the state bordering Oregon and Nevada, including far northern parts of the Central Valley and the Sierra Nevada mountain range. Historically, the Shasta Cascade region was home to Native Americans of the Modoc, Maidu, Okwanuchu, Paiute, Shasta, Wintu, and Yana tribes, and sub-groups of those tribes. The first non-Native Americans entered the Shasta Cascade region by coming south along the Siskiyou Trail from Oregon, or north along the Siskiyou Trail from central California or the San Francisco Bay Area. These earliest explorers were

neg: Mount Aix east of Mount Rainier National Park, north of Goat Rocks Wilderness, west of Yakima, and south of Mount Daniel (Alpine Lakes Wilderness), so it is quite prominent. Prior to 1897 (when Mount Aix was officially recognized by the USGS) the name was spelled as Mount Aiks on early survey maps and publications. Mount Aix is located east of the Cascade crest. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the

neg: Okanagan Range lower Ashnola River. Peakbagger.com defines the Okanogan Range as a much larger region bounded to the south by the Methow River and to the east by the Okanagan River and Similkameen River. The Okanagan Range should not be confused with the Okanagan Highland, which is located on the farther side of the Okanagan Valley and is sometimes classified as part of the Monashee Mountains. Okanagan Range The Okanagan Range or Okanogan Range is a small subrange of the Cascade Range straddling the border between British Columbia and Washington south of the Similkameen River on the inland side of the range.

neg: McClellan Peak McClellan Peak McClellan Peak is a 8,364 ft summit located in Chelan County of Washington state. Its name honors Army explorer George B. McClellan who visited the area in 1853. McClellan Peak is part of The Enchantments within the Alpine Lakes Wilderness, and it belongs to the Stuart Range which is subset of the Cascade Range. McClellan Peak is situated 1.29 miles east of Little Annapurna which is its nearest higher peak. Precipitation runoff drains into tributaries of the Wenatchee River. Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Mountains. As fronts approach, they

neg: Enchantment Peak Enchantment Peak Enchantment Peak is an 8520+ ft granite summit located in Chelan County of Washington state. Enchantment Peak is part of The Enchantments within the Alpine Lakes Wilderness. Enchantment Peak belongs to the Stuart Range which is subset of the Cascade Range. Enchantment Peak is situated midway between Prusik Peak to its east, and Aasgard Pass and Dragontail Peak to the west. Precipitation runoff drains into Icicle Creek, a tributary of the Wenatchee River. Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks

neg: Stevens Peak there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. Stevens Peak Stevens Peak is a summit in the Tatoosh Range which is a sub-range of the Cascade Range. It's located in Mount Rainier National Park, one mile east of Unicorn Peak. The name honors Hazard Stevens who made the first documented ascent of Mount Rainier along with P. B. Van Trump on August 17, 1870. Precipitation runoff from the mountain drains into tributaries of the Cowlitz River. Stevens Peak is located in

neg: Eagle Peak (Washington) Eagle Peak (Washington) Eagle Peak is a summit on the west end of the Tatoosh Range which is a sub-range of the Cascade Range. It's located south of Mount Rainier within Mount Rainier National Park, and immediately east of Longmire. Eagle Peak was originally known as "Simlayshe", a Native American word meaning "eagle". George Longmire anglicized the name to Eagle Peak. The four mile Eagle Peak Trail leads to views of Mount Rainier. The summit of Eagle Peak requires scrambling. Precipitation runoff on the peak drains into the Nisqually River. Eagle Peak is located in the marine west coast climate

neg: Holden Village, Washington Holden Village, Washington Holden Village is a year-round Lutheran Christian center in the North Cascade mountains of the U.S. state of Washington. Formerly the site of one of the largest copper mines in the United States, the Holden mine, Holden is accessible only by the Lake Chelan passenger ferry, the "Lady of the Lake", or by hiking in through the Cascade Mountains. Holden Village is the largest retreat center in the nation operating under a special use permit from the United States Department of Agriculture - Forest Service. Holden Village is located in the Cascade Range in Washington, in the

neg: North American Cordillera (and was the first-named of these groupings). The Cascade Range (called the Cascade Mountains in Canada) extends from northern California in the United States to British Columbia, Canada. It consists of non-volcanic and volcanic mountains: all of the known historic eruptions in the contiguous United States have been from the volcanoes of the Cascade Volcanic Arc. The highest peak in the Cascade Range is Mount Rainier (), a stratovolcano. The small portion of the Cascade Range in Canada is called the Cascade Mountains or Canadian Cascades, and in its southwestern area is similar in terrain to the area north of

neg: Ecology of the North Cascades Ecology of the North Cascades The Ecology of the North Cascades is heavily influenced by the high elevation and rain shadow effects of the mountain range. The North Cascades is a section of the Cascade Range from the South Fork of the Snoqualmie River in Washington, United States, to the confluence of the Thompson and Fraser Rivers in British Columbia, Canada, where the range is officially called the Cascade Mountains but is usually referred to as the Canadian Cascades. The North Cascades Ecoregion is a Level III ecoregion in the Commission for Environmental Cooperation's classification system. The terrain of the

neg: Chuckanut Mountains Chuckanut Mountains The Chuckanut Mountains (from "Chuckanut", a native word for "Long beach far from a narrow entrance"), or Chuckanuts, are located on the northern Washington state coast of the Salish Sea, just south of Bellingham, Washington. Being a part of the Cascade Range, they are the only place where the Cascades come west down to meet the sea. The Chuckanuts are considered to be a part of the Puget Lowland Forest Ecoregion. The range contains Larrabee State Park, the first State Park to be designated in Washington (1923). Its mountains include: The Chuckanut Mountains were formed by the folding

neg: Cutthroat Peak Cutthroat Peak Cutthroat Peak is a granitic mountain located on the boundary of Chelan County and Skagit County, in Washington. The mountain is part of the Okanagan Range in the Cascade Range. Cutthroat Peak is about two miles west of Washington Pass and one mile east of Rainy Pass. It's a prominent landmark along the North Cascades Highway. There is also a Cutthroat Lake, Cutthroat Creek, and Cutthroat Pass on its north and east aspects. Molar Tooth is a granite pillar half a mile north on the ridge extending to Cutthroat Pass. Cutthroat Peak is located in the marine west

neg: Fraser River From Lytton southwards it runs through a progressively deeper canyon between the Lillooet Ranges of the Coast Mountains on its west and the Cascade Range on its east. Hell's Gate, located immediately downstream of the town of Boston Bar, is a famous portion of the canyon where the walls narrow dramatically, forcing the entire volume of the river through a gap only 35 metres (115 feet) wide. An aerial tramway takes visitors out over the river. Hells Gate is visible from the Trans-Canada Highway 1 about south of the tramway. Simon Fraser was forced to portage the gorge on his

neg: Burlington Northern Railroad Montana Rail Link in 1987), crossing the continental divide at Mullan and Homestake Passes. At Spokane the routes split into three. The former Great Northern route ran west to Wenatchee, Washington, crossed under the Cascade Range at New Cascade Tunnel on Stevens Pass, and descended to the Puget Sound region through Everett, Washington. The former Northern Pacific turned southwest towards the Tri-Cities, then northwest to Yakima, Washington, and crossed under the Cascade Range at Stampede Tunnel, descending to the Green River Valley at Auburn, Washington where it connected with existing NP lines from British Columbia to Portland, Oregon. The Spokane,

neg: Bismarck Peak Peak drains into tributaries of the Yakima River, thence into the Columbia River. Bismarck Peak is located east of the Cascade crest. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the east side of the Cascades experiences less precipitation than the west side of the crest. During winter months, weather is usually cloudy, but, due to high pressure

neg: Union Peak Union Peak Union Peak is a heavily eroded shield volcano in the Cascade Range of central Oregon, located along the Cascade Crest less than southwest of the rim of Crater Lake. Ice Age glaciers eroded away most of the flanks of the volcano, leaving numerous deep cirques surrounding a central glacial horn. This is the same process that formed the summit horns of Three Fingered Jack, Mount Washington, Howlock Mountain, and Mount Thielsen from other shield volcanoes farther north in the Oregon Cascades. Union Peak is located within Crater Lake National Park, and the summit was used as a post

neg: Dynamical system (definition) "discrete-time dynamical system", "map" or "cascade" is a tuple (T, M, Φ) where T is the set of integers, M is a manifold locally diffeomorphic to a Banach space, and Φ is a function. If T is restricted to the non-negative integers we call the system a "semi-cascade". A "cellular automaton" is a tuple (T, M, Φ), with T a lattice such as the integers or a higher-dimensional integer grid, M is a set of functions from an integer lattice (again, with one or more dimensions) to a finite set, and Φ a (locally defined) evolution function. As such cellular

neg: Cascade Mountain (Utah) Cascade Mountain (Utah) Cascade Mountain is located in central Utah (Utah County just east of Provo and Orem Utah). With an elevation of , it is not as high as its neighbors, to the north Mount Timpanogos () and Provo Peak () to the south, but it is one of the major peaks of the Wasatch Range. There are several access routes to the summit. The safest and easiest routes are either from the Dry Fork trail that starts at the Rock Canyon Campground to the south west of the mountain or the Big Springs trails from the east. There

neg: Cascade Mountain (Utah) are many other routes from Bridal Veil Falls or the western side of the mountain but they are much more difficult and should be used by experienced hikers. Cascade Mountain (Utah) Cascade Mountain is located in central Utah (Utah County just east of Provo and Orem Utah). With an elevation of , it is not as high as its neighbors, to the north Mount Timpanogos () and Provo Peak () to the south, but it is one of the major peaks of the Wasatch Range. There are several access routes to the summit. The safest and easiest routes are either

neg: Mount Jefferson Wilderness Pacific Crest Trail. Mount Jefferson Wilderness The Mount Jefferson Wilderness is a wilderness area located on and around Mount Jefferson in the central Cascade Range of Oregon in the United States. It is situated where the Willamette, Deschutes, and Mount Hood National Forests meet. Mount Jefferson Wilderness is the second most visited Oregon wilderness area after the Three Sisters Wilderness. At , Mount Jefferson is the second tallest mountain in Oregon. It is a stratovolcano with slopes mantled by five glaciers - Whitewater, Waldo, Milk Creek, Russell, and Jefferson Park. Three Fingered Jack is a heavily eroded and deeply glaciated

neg: Mount Jefferson Wilderness Mount Jefferson Wilderness The Mount Jefferson Wilderness is a wilderness area located on and around Mount Jefferson in the central Cascade Range of Oregon in the United States. It is situated where the Willamette, Deschutes, and Mount Hood National Forests meet. Mount Jefferson Wilderness is the second most visited Oregon wilderness area after the Three Sisters Wilderness. At , Mount Jefferson is the second tallest mountain in Oregon. It is a stratovolcano with slopes mantled by five glaciers - Whitewater, Waldo, Milk Creek, Russell, and Jefferson Park. Three Fingered Jack is a heavily eroded and deeply glaciated shield volcano and

neg: Sky Lakes Wilderness Sky Lakes Wilderness The Sky Lakes Wilderness is a wilderness area located in the Rogue River–Siskiyou and Fremont–Winema national forests in the southern Cascade Range of Oregon in the United States. It comprises , of which are in the Rogue River–Siskiyou National Forest and are in the Fremont–Winema National Forest. It was established in 1984 under the Wilderness Act of 1964. The Sky Lakes Wilderness straddles southern Oregon's Cascade Range from Crater Lake National Park southward to Oregon Route 140. It is approximately wide and long, with elevations ranging from in the canyon of the Middle Fork of the Rogue

neg: Olympic-Wallowa Lineament but this has not been observed. The interaction of the Straight Creek Fault with the OWL has yielded practically no intelligible information, and remains as enigmatic as the OWL itself. More informative is the closely related Darrington—Devils Mountain Fault Zone (DDMFZ). It runs east from a complex of faults on the southern end of Vancouver Island to the town of Darrington, where it turns south to converge with the SCF (see map, above). North of the DDMFZ (and west of the SCF) is the Chuckanut Formation (part of the "Northwest Cascade System" of rocks shown in green on the map),

neg: Mount Mazama Mount Mazama Mount Mazama ("Giiwas" in the Native American language Klamath) is a complex volcano in the Oregon segment of the Cascade Volcanic Arc and the Cascade Range, in the United States, that was destroyed due to a major eruption that took place 7,700 years ago. Located in Klamath County, the volcano resides to the north of the border between Oregon and California in the southern Cascades. Its collapsed caldera holds Crater Lake, and the entire mountain is located within Crater Lake National Park. Mazama has an elevation of 8,157 feet (2,486 m) and Crater Lake reaches a depth of

neg: High Desert (Oregon) High Desert (Oregon) The Oregon high desert is a region of the U.S. state of Oregon located east of the Cascade Range and south of the Blue Mountains, in the central and eastern parts of the state. Divided into a southern region and a northern region, the desert covers most of five Oregon counties and averages above sea level. The southwest region is part of the Great Basin and the southeast is the lower Owyhee River watershed. The northern region is part of the Columbia Plateau, where higher levels of rainfall allow the largest industry on private land to be

neg: Wallaman Falls Wallaman Falls The Wallaman Falls, a cascade and horsetail waterfall on the Stony Creek, is located in the UNESCO World Heritagelisted Wet Tropics in the northern region of Queensland, Australia. The waterfall is notable for its main drop of , which makes it the country's tallest single-drop waterfall. The pool at the bottom of the waterfall is deep. An estimated people visit the waterfall annually. The waterfall is situated in the Girringun National Park as it descends from the Atherton Tableland, where the Stony Creek, a tributary of the Herbert River, flows over an escarpment in the Seaview Range. The

neg: Tumalo Creek Tumalo Creek Tumalo Creek is a tributary, about long, of the Deschutes River, located in Deschutes County in Central Oregon, United States. It rises in the Cascade Range at , where Middle Fork Tumalo Creek and North Fork Tumalo Creek meet, and forms several waterfalls, including the Tumalo Falls. Its mouth is on the Deschutes at . It is home to several species of trout, including the Columbia River redband trout. It is the primary drinking water source for the city of Bend. The lower reaches of the creek are often emptied for irrigation, drained by a tunnel flume at

neg: Perideridia erythrorhiza Perideridia erythrorhiza Perideridia erythrorhiza is a rare species of flowering plant in the carrot family known by the common names western yampah and redroot yampah. It is endemic to Oregon in the United States, where there are about 20 occurrences. The populations occur in three regions in southwestern Oregon which are separated by more than 50 miles. The three separate groups are located in the Klamath Mountains and on either side of the Cascade Range. This plant is a perennial herb growing up to 1.2 meters in height. The roots are pink to reddish brown in color. The inflorescence is

neg: Geography of California The Cascades (as they are called for short) are part of the Pacific Ring of Fire, the ring of volcanoes around the Pacific Ocean. All of the known historic eruptions in the contiguous United States have been from either Cascade volcanoes or near Mono Lake. Lassen Peak was the last Cascade volcano to erupt in California, from 1914 to 1921. Lassen is the most southerly active volcano of the Cascade chain. This region is located in the northeastern section of the state bordering Oregon and Nevada, mostly north of the Central Valley and the Sierra Nevada mountain range. The area

neg: Mount St. Helens Mount St. Helens Mount St. Helens or Louwala-Clough (known as Lawetlat'la to the indigenous Cowlitz people, and Loowit to the Klickitat) is an active stratovolcano located in Skamania County, Washington, in the Pacific Northwest region of the United States. It is northeast of Portland, Oregon and south of Seattle, Washington. Mount St. Helens takes its English name from the British diplomat Lord St Helens, a friend of explorer George Vancouver who made a survey of the area in the late 18th century. The volcano is located in the Cascade Range and is part of the Cascade Volcanic Arc, a segment

neg: Mount Rainier Mount Rainier Mount Rainier (pronounced: ), also known as Tahoma or Tacoma, is the highest mountain of the Cascade Range of the Pacific Northwest, and the highest mountain in the U.S. state of Washington. It is a large active stratovolcano located south-southeast of Seattle, in the Mount Rainier National Park. It is the most topographically prominent mountain in the contiguous United States and the Cascade Volcanic Arc, with a summit elevation of . Mt. Rainier is considered one of the most dangerous volcanoes in the world, and it is on the Decade Volcano list. Because of its large amount of

neg: Cascade Locks Historic District Cascade Locks Historic District The Cascade Locks Historic District is a historic district located in Akron, Ohio. It was added to the National Register of Historic Places in 1992. Located immediately northwest of downtown Akron, the Cascade Locks Historic District is a ravine that opens up to a flat plane where the Ohio and Erie Canal empties into the Little Cuyahoga River. This area of the canal included the steepest grade of the entire 304 miles between Lake Erie to the Ohio River. The district was the site of many industrial operations during the 19th and early 20th centuries, fueled