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| Lakes, Rivers, Inlets | Preview | Description |
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Washington |
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The Alpine Lakes is the largest Wilderness area near the population centers of Puget Sound, at approximately 394,000 acres (1600 square km). It is located on the Cascade Range between Interstate 90 (Snoqualmie Pass) and US Route 2 (Stevens Pass). Bald Eagle Peak dominates this scene in the northern center of the print standing 6,230 feet (1,899 meters). Snow clad Mount Hinman at 7,492 feet (2,284 meters) on the eastern side of this print, is the birthplace of Hinman and Lynch Glaciers, and the beginning of the Middle Fork Snoqualmie River in the Dutch Miller Gap (southwest). The northern ridgeline of the gap is home to Iron Cap Mountain and Big Snow Mountain. The dozens of lakes in this region give the name to the Wilderness. From the northwestern lake, going southeasterly: Panorama Lake, Purvis Lake, Lake Malachite, Cooper Lake, Little Heart Lake, Delta Lake, Big Heart Lake, Angeline Lake, Otter Lake, Azurite Lake, Chetwoot Lake, Gold Lake, and Crawford Lake. From the summit of Bald Eagle Peak, southerly, Nazanne Lake, Jewell Lake, Lochet Lake, Al Lake, Hade Lake, Lake Ilswoot, Emerald Lake, Tahl Lake, Opal Lake, La Bahn Lake, and Williams Lake. | | ||||||||||||
Washington |
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Bainbridge Island, located on Puget Sound, Washington, is featured along with a portion of the Kitsap Peninsula cities of Bremerton, Silverdale, and Port Orchard. | | ||||||||||||
Washington |
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Sinclair Inlet, Dyes Inlet, Port Washington Narrows, Bremerton, Silverdale, Manette, Tracyton, Gorst, Port Orchard, Manchester, and Colby, Washington. | | ||||||||||||
Idaho |
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Including the communities of (from south to north): Charcolet, Ramsdell, Heyburn, Conkling Park, Harrison, Medimont, Whorley, Bellgrove, Mica, Twin Beaches, Eddyville, Coeur d'Alene, Fernan, Huetter, Post Falls, and Wolf Lodge. | | ||||||||||||
Oregon |
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Crater Lake caldera (8,156 feet, 2,487 meters) was formed by a collapse during the catastrophic eruption of approximately 12 cubic miles (50 cubic kilometers) of magma, 6,845 years ago. The 5 mile by 6 mile (8x10 kilometer) caldera lies in the remains of Mount Mazama, a Pleistocene stratovolcano cluster covering 150 square miles (400 square kilometers) in the southern Oregon Cascades. Prior to its climactic eruption, Mount Mazama's summit had an elevation between 10,800 feet and 12,000 feet (3,300 meters and 3,700 meters). Its southern and southeastern flanks were deeply incised by glacial valleys, now beheaded, that form U-shaped notches in the caldera wall. Crater Lake reaches a maximum depth of 1,932 feet (588 meters). Wizard Island Post-caldera volcanic landforms are present beneath the lake surface and poke through to form Wizard Island. The central platform, Merriam Cone, and Wizard Island are all andesite evidently erupted within a few hundred years of caldera's collapse. | | ||||||||||||
Washington |
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Hood Canal's southern half and Case Inlet's northern reaches. Also included are the populated places of Belfair, Union, Hoodsport, Potlatch, Lilliwap, Allyn, Victor, Dewatto, Tahuya, Grapeview, Vaughn, and the Skokomish Indian Reservation, Washington. Past glaciation is clearly evident across the entire landscape. | | ||||||||||||
Washington |
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Located on the Olympic Peninsula at the gateway to the Olympic National Park at the Staircase Campground. | | ||||||||||||
Washington |
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Makah Indian Reservation, Neah Bay, Makah Bay, Tatoosh Island, Pacific Ocean, Strait of Juan de Fuca, Northwestern Washington. Tatoosh is an island about one-half mile northwest of Cape Flattery on the Olympic Peninsula. This region is at the most northwestern corner of the continental United States, the Makah Indian Reservation, and is part of Clallam County, Washington. The Pacific Ocean lies to the west while the Strait of Juan de Fuca begins to the north and east providing access to Puget Sound and the protected ports of Washington and British Columbia, Canada. Makah Bay rests on the Pacific Ocean side of the peninsula, while Neah Bay is protected on the northern flanks. Tatoosh Island has been home to a lighthouse since December 28, 1857, built by the US Coast Guard. | | ||||||||||||
Oregon |
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Mount Bailey (8,363 feet, 2,549 meters) is the southernmost volcano in a north-south-trending volcanic chain 6 miles (10 kilometers) long that rises west of Diamond Lake. Mount Bailey is about the same age as Diamond Peak, 27 miles (43 kilometers) north. Like Diamond Peak, Mount Bailey consists of a tephra cone surrounded by basaltic andesite lava. Bailey is slightly smaller 2.0-2.2 cubic miles (8-9 cubic kilometers) than Diamond Peak, and minor andesite erupted from the summit cone in its late stages, whereas Diamond Peak eruptions were never more siliceous than basaltic andesite. | | ||||||||||||
Washington |
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Mount Si (pronounced sigh) is a small mountain in the US state of Washington. Although just 4,167 ft (1,270 meter) high, it lies on the western margin of the Cascade Range just above the coastal plains around Puget Sound, and towers over the nearby town of North Bend. The mountain was named after local homesteader Josiah "Uncle Si" Merritt. It was made famous in the show Twin Peaks, which was filmed in North Bend and Snoqualmie. Mt. Si is a remnant of an oceanic plate volcano and the rocks are highly metamorphosed. Related to the Indian legend and seeing that the rock of Mt. Si is indeed 'foreign' rock and not like that of the surrounding countryside it might, perhaps, be that the Indians had recognized this fact and attempted to explain it with the story of the Moon falling to earth. The communities of North Bend, Snoqualmie, and Fall City, Washington, are also included around the three forks of the Snoqualmie River (North, Middle, and South Forks). | | ||||||||||||
Washington |
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Mount Stuart at 9,415 feet (2,869 meters) is located in the Cascade Range and is the second highest non-volcanic peak in the state, after nearby Bonanza Peak. It is the sixth-highest independent peak in Washington overall. Mount Stuart is the highest peak in the Stuart Range, and is contained within the Alpine Lakes Wilderness, located in the central part of the Washington Cascades, south of Stevens Pass and east of Snoqualmie Pass. Like many Cascade peaks, Mount Stuart is more notable for its local relief than for its absolute elevation. For example, the south face rises 5000 feet (1524 m) in just 2 horizontal miles (3.2 km). The northeast and northwest sides of the mountain exhibit similar steep relief. The rock of Mount Stuart is unusually rugged and unstable, due to the extensive jointing of the granite. The Stuart Glacier, Sherpa Glacier, and the Ice Cliff Glacier flow from the summit of Mount Stuart. Other high points on this print include (from west to east) Ingalis Peak, Sherpa Peak, Argonaut Peak, Colchuck Peak, and Dragontail Peak. | | ||||||||||||
Oregon |
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Mount Thielsen (9,182 feet, 2,799 meters) is a shield volcano comprising approximately 2 cubic miles (8 cubic kilometers) of basaltic andesite built atop a broad pedestal of older lava. Thielsen is remarkable even at a distance for its colorfully interbedded pyroclastic rocks that dip away from the jagged spire of the central plug, often called the "lightning rod of the Cascades". The most spectacular views are on the north and east sides (accessible only by foot or horseback) where now-vanished glaciers have carved precipitous cirque walls that reveal the construction. Thielsen's age is approximately 290,000 years, and its geomorphology is a reference point for assigning Cascade Range volcanoes to the age division 0-0.25 million years (younger than Thielsen) or 0.25-0.73 million years (older than Thielsen). | | ||||||||||||
Oregon |
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Newberry Volcano, centered about 20 miles (32 km) southeast of Bend, Oregon, is among the largest Quaternary volcanoes in the conterminous United States. It covers an area in excess of 500 square miles (1,300 square km), and lava from it extends northward many tens of miles. The highest point on the volcano, Paulina Peak with an elevation of 7,984 feet (2,433 meters), is about 4,000 feet (1,219 meters) higher than the terrain surrounding the volcano. The gently sloping flanks, embellished by more than 400 cinder cones, consist of basalt and basaltic andesite flows, andesitic to rhyolitic ash-flow and air-fall tuffs and other types of pyroclastic deposits. At Newberry's summit is a 4- to 5-mile-wide (6-8 km) caldera that contains scenic Paulina Lake and East Lake. The caldera has been the site of numerous Holocene eruptions, mostly of rhyolitic composition, that occurred as recently as 1,400 years ago. | | ||||||||||||
Washington |
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Orcas Island is the largest of the San Juan Islands, which are located in the northwestern corner of Washington state in San Juan County. Orcas Island is slightly larger, but less populous, than neighboring San Juan Island. Orcas is shaped like a pair of saddlebags, separated by fjord-like East Sound, with Massacre Bay on the south side, and tiny Skull Island just off the coast. At the northern end of East Sound is the village of Eastsound. In 1989 the Lummi Indian Nation regained a village and burial site on Orcas Island's Madrona Point near Eastsound. Mount Constitution is a 2,409 foot high (734 m) mountain on Orcas Island. It is the highest point on any of the San Juan Islands. At the summit there stands a stone observation tower built by the Civilian Conservation Corps in 1936. Also mapped are Shaw Island (southwest of Orcas Island), Blakely Island (southeast), Obstruction Island (between Orcas and Blakely), the northern tip of Lopez Island (south of Orcas), and Crane Island (between Orcas and Shaw). The very small islands northeast of Orcas are Barnes and Clark Islands. A portion of Waldron Island is visible in the northwest corner of this map. | | ||||||||||||
Alaska |
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Portage Glacier is located on the Kenai Peninsula of Alaska and is included within the Chugach National Forest. It is located south of Portage Lake and 4 miles (6 km) west of Whittier. Portage Glacier was a local name first recorded in 1898 by Thomas Corwin Mendenhall of the U.S. Coast and Geodetic Survey, so called because it is on a portage route between Prince William Sound and Turnagain Arm. Portage Glacier feeds Portage Lake (705 feet, 215 meters) from the southwest where it flows from Carpathian Peak (4,501 feet, 1,372 meters) pictured here. | | ||||||||||||
Washington |
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The San Juan Islands are a part of the San Juan Archipelago in the northwest corner of the continental United States. San Juan Island is the second-largest and most populous of these Islands. It has a land area of 55.053 sq mi (142.59 km²). The name "San Juan" comes from the 1791 expedition of Francisco de Eliza, who named the archipelago Isla y Archiepelago de San Juan to honor his patron, Juan Vicente de Güemes Padilla Horcasitas y Aguayo, 2nd Count of Revillagigedo. One of the officers under Eliza's command, Gonzalo López de Haro, was the first European to discover San Juan Island itself. The American explorer Charles Wilkes renamed the island Rodgers Island, but the Spanish name was kept on British charts and became the standard. Mount Dallas stands on the western side of the Island at 1,086 feet (331 meters). | | ||||||||||||
Washington |
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Puget Sound, Lake Washington, Lake Sammamish, Seattle, Bellevue, Issaquah, Mercer Island, Sammamish, University of Washington, Redmond, Kirkland, Medina. | | ||||||||||||
Washington |
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Snoqualmie Mountain, at 6,278 feet (1,914 meters) above sea level, is the tallest peak in the immediate vicinity of Snoqualmie Pass in the Cascade Range of Washington state. Its shape is often described as "amorphous" or "blob-like", although it does display a steep north face dropping down to the Middle Fork of the Snoqualmie River. The boundary of the Alpine Lakes Wilderness crosses the summit of Snoqualmie Mountain. It appears due north of Snoqualmie Pass (Interstate 90), and east of Snow Lake. Adjacent to Snoqualmie Mountain, moving eastward, are Lundin Peak, Red Mountain, then south along the ridgeline is Kendall Peak. Due west of Snoqualmie Pass is Denny Mountain, then northwesterly along the ridgeline is Bryant Peak, Chair Peak, and Melakwa Peak (just west of Snow Lake). | | ||||||||||||
Washington |
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This print provides an unique view of the Spokane River through the downtown Spokane area, where it turns to the northwest and meanders against the ridgelines to the west where the Spokane Airport is located. | | ||||||||||||
Washington |
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Puget Sound, Port of Tacoma, Tacoma, Ruston, Monta Vista, Lakewood, Fife, Milton, Lakota, Caledonia, Titlo, Oakland, Hillsdale, Fort Nisqually, Brown's Point, Tacoma Narrows, Dash Point, and Sunset Beach, Washington. | | ||||||||||||
| Mountains | Preview | Description |
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Washington |
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The Alpine Lakes is the largest Wilderness area near the population centers of Puget Sound, at approximately 394,000 acres (1600 square km). It is located on the Cascade Range between Interstate 90 (Snoqualmie Pass) and US Route 2 (Stevens Pass). Bald Eagle Peak dominates this scene in the northern center of the print standing 6,230 feet (1,899 meters). Snow clad Mount Hinman at 7,492 feet (2,284 meters) on the eastern side of this print, is the birthplace of Hinman and Lynch Glaciers, and the beginning of the Middle Fork Snoqualmie River in the Dutch Miller Gap (southwest). The northern ridgeline of the gap is home to Iron Cap Mountain and Big Snow Mountain. The dozens of lakes in this region give the name to the Wilderness. From the northwestern lake, going southeasterly: Panorama Lake, Purvis Lake, Lake Malachite, Cooper Lake, Little Heart Lake, Delta Lake, Big Heart Lake, Angeline Lake, Otter Lake, Azurite Lake, Chetwoot Lake, Gold Lake, and Crawford Lake. From the summit of Bald Eagle Peak, southerly, Nazanne Lake, Jewell Lake, Lochet Lake, Al Lake, Hade Lake, Lake Ilswoot, Emerald Lake, Tahl Lake, Opal Lake, La Bahn Lake, and Williams Lake. | | ||||||||||||
California |
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Black Butte (6,245 feet, 1,903 meter) is a group of dacite domes located about 8 miles (13 km) southwest of Mount Shasta. It is a landmark for the surrounding communities of Upton, Deetz, and Black Butte, and is also a monument for travelers of Interstate-5. These domes were formed about 9,500 years ago as a flank vent of Mount Shasta and was part of the larger mountain's eruptive activity. | | ||||||||||||
Oregon |
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Crater Lake caldera (8,156 feet, 2,487 meters) was formed by a collapse during the catastrophic eruption of approximately 12 cubic miles (50 cubic kilometers) of magma, 6,845 years ago. The 5 mile by 6 mile (8x10 kilometer) caldera lies in the remains of Mount Mazama, a Pleistocene stratovolcano cluster covering 150 square miles (400 square kilometers) in the southern Oregon Cascades. Prior to its climactic eruption, Mount Mazama's summit had an elevation between 10,800 feet and 12,000 feet (3,300 meters and 3,700 meters). Its southern and southeastern flanks were deeply incised by glacial valleys, now beheaded, that form U-shaped notches in the caldera wall. Crater Lake reaches a maximum depth of 1,932 feet (588 meters). Wizard Island Post-caldera volcanic landforms are present beneath the lake surface and poke through to form Wizard Island. The central platform, Merriam Cone, and Wizard Island are all andesite evidently erupted within a few hundred years of caldera's collapse. | | ||||||||||||
Oregon |
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Diamond Peak (8,750 feet, 2,667 meters), the dominant landform in the Willamette Pass area, is a basaltic andesite shield approximately 3.6 cubic miles (15 cubic kilometers) in volume. Like other shields in the area, it has a central pyroclastic cone that is surrounded and surmounted by lava flows. Diamond Peak began erupting from a vent near its northern summit. A second vent later opened near the southern summit, piggy-backing its lava and tephra over the previously erupted volcanic rocks. This vent migration likely involved only a small interval of time. Diamond Peak is probably less than 100,000 years old, but is certainly older than the last glaciation, which ended approximately 11,000 years ago. | |