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Garfield Peak (Oregon)
Garfield Peak is a mountain peak on the south end of Crater Lake in Crater Lake National Park, Oregon. The top of the peak reaches above sea level. The peak has a elevation trail to the summit from the Crater Lake lodge, one of the most popular hiking sites surrounding the lake. The trail continues east toward Applegate peak ( high). The peak is one of seven peaks on Crater Lake's rim to rise above . History The Garfield Peak was named in honor of James Rudolph Garfield, the Secretary of Interior for President Theodore Roosevelt, who created the national park in 1902. Garfield visited the park in 1907, the first cabinet member to visit Crater Lake. Geology Garfield Peak was created after Mount Mazama, a large stratovolcano, erupted violently approximately 7,700 years ago, formed on the rim of its caldera which now contains Crater Lake. The walls along the southern rim of Crater Lake have had a peculiar influence from sulfur steams coming off fumaroles, which color the r ...
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Crater Lake Lodge
Crater Lake Lodge is a hotel built in 1915 to provide overnight accommodations for visitors to Crater Lake National Park in southern Oregon, US. The lodge is located on the southwest rim of the Crater Lake caldera overlooking the lake below. The lodge is owned by the National Park Service, and is listed on the National Register of Historic Places. In 2022, the hotel is a Historic Hotels of America program member, and has been so since 2012. Local history Crater Lake lies inside a caldera created 7,700 years ago when the -high Mount Mazama collapsed following a large volcanic eruption. Over the following millennium, the caldera was filled with rain water forming today's lake."Crater Lake - Like No Place Else on Earth"
Crater Lake National Park, National Park Service, United States Department of Interior, March 8, 2008.
The Klam ...
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Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ...
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Crater Lake Garfield Peak Trail View East
Crater may refer to: Landforms * Impact crater, a depression caused by two celestial bodies impacting each other, such as a meteorite hitting a planet * Explosion crater, a hole formed in the ground produced by an explosion near or below the surface ** Subsidence crater, a depression from an underground (usually nuclear) explosion * Pit crater, a crater that forms through sinking of the surface and not as a vent for lava * Volcanic crater, a roughly circular depression in the ground caused by volcanic activity **Caldera, a large cauldron-like depression formed following the evacuation of a magma chamber/reservoir **Maar, a type of volcanic crate caused by a phreatic eruption or explosion ** Volcanic crater lake, including a list of lakes that formed in a volcanic or impact crater Music * ''Crater'' (Daniel Menche and Mamiffer album), 2016 * Crater (Fission album), 2004 Places *Crati or Crater, a river of southern Italy * Crater, California, U.S. * Crater (Aden), a district of the ...
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Ribes Laxiflorum
''Ribes laxiflorum'' is a species of currant known by the common names trailing black currant, and spreading currant. It is native to western North America. Description ''Ribes laxiflorum'' is a spreading, trailing shrub usually growing in height. It has been known to take a somewhat vine-like form in appropriate shady habitat with nearby supports, climbing to in length. It has fuzzy, glandular stems lacking spines and prickles. The hairy, glandular, maple-shaped leaves are up to long and deeply divided into several pointed lobes lined with dull teeth. The inflorescence is a mostly erect raceme of up to eight flowers. The distinctive flower has five greenish, purplish, or red sepals which are often curved back at the tips. At the center is a corolla of five red or pink petals each measuring long, narrow at the base and wider or club-shaped at the tip. Inside the corolla are five red stamens tipped with whitish anthers. The fruit is a purple-black berry measuring wide which i ...
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Dark-eyed Junco
The dark-eyed junco (''Junco hyemalis'') is a species of junco, a group of small, grayish New World sparrows. This bird is common across much of temperate North America and in summer ranges far into the Arctic. It is a very variable species, much like the related fox sparrow (''Passerella iliaca''), and its systematics are still not completely untangled. Taxonomy The dark-eyed junco was formally described by the Swedish naturalist Carl Linnaeus in his landmark 1758 10th edition of ''Systema Naturae'' as ''Fringilla hyemalis''. The description consisted merely of the laconic remark "''F ingillanigra, ventre albo.'' ("A black 'finch' with white belly") and a statement that it came from America. Linnaeus based his description on the "Snow-Bird" that Mark Catesby had described and illustrated in his ''The Natural History of Carolina, Florida and the Bahama Islands''. The Bill of this Bird is white: The Breast and Belly white. All the rest of the Body black; but in some places dusky, ...
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Yellow-bellied Marmot
The yellow-bellied marmot (''Marmota flaviventris''), also known as the rock chuck, is a large, stout-bodied ground squirrel in the marmot genus. It is one of fourteen species of marmots, and is native to mountainous regions of southwestern Canada and western United States, including the Rocky Mountains, Sierra Nevada, and Mount Rainier in the state of Washington, typically living above . The fur is mainly brown, with a dark bushy tail, yellow chest and white patch between the eyes, and they weigh up to approximately . They live in burrows in colonies of up to twenty individuals with a single dominant male. They are diurnal and feed on plant material, insects, and bird eggs. They hibernate for approximately eight months starting in September and lasting through the winter. Description Yellow-bellied marmots usually weigh from when fully grown, though males typically weigh more than females. The weight fluctuates quite drastically through the year, with the least measured in ea ...
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American Pika
The American pika (''Ochotona princeps''), a diurnality, diurnal species of pika, is found in the mountains of western North America, usually in boulder fields at or above the tree line. They are herbivorous, smaller relatives of rabbits and hares. Pikas have two different ways of foraging; they either directly consume food or they cache food in piles for the winter (haying). Pikas are vocal, using both calls and songs to warn when predators are nearby and during the Estrous cycle, breeding season. Predators of the pika include eagles, hawks, coyotes, bobcats, foxes, and weasels. Recent studies suggest some populations are declining due to habitat loss and global warming. They generally cannot tolerate temperatures above . Currently the American pika is considered a species of least concern. Description American pikas, known in the 19th century as "little Chief hares", have a small, round, ovate body. Their body lengths range from . Their hind feet range from 25 to 35 mm ...
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Abies Lasiocarpa
''Abies lasiocarpa'', the subalpine fir or Rocky Mountain fir, is a western North American fir tree. Description ''Abies lasiocarpa'' is a medium-sized evergreen conifer with a very narrow conic crown, growing to tall, exceptionally , with a trunk up to thick, exceptionally . The bark on young trees is smooth, gray, and with resin blisters, becoming rough and fissured or scaly on old trees. The lowest branches can be observed growing above ground level. The leaves are flat and needle-like, long, glaucous green above with a broad stripe of stomata, and two blue-white stomatal bands below; the fresh leaf scars are reddish (tan on the inland variety). They are arranged spirally on the shoot, but with the leaf bases twisted to be arranged to the sides of and above the shoot, with few or none below the shoot. The cones are erect, long, dark purple with fine yellow-brown pubescence, ripening brown and disintegrating to release the winged seeds in early fall. Taxonomy There are ...
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Pinus Albicaulis
''Pinus albicaulis'', known by the common names whitebark pine, white bark pine, white pine, pitch pine, scrub pine, and creeping pine, is a conifer tree native to the mountains of the western United States and Canada, specifically subalpine areas of the Sierra Nevada, Cascade Range, Pacific Coast Ranges, and Rocky Mountains. It shares the common name "creeping pine" with Creeping pine, several other plants. The whitebark pine is typically the highest-elevation pine tree found in these mountain ranges and often marks the tree line. Thus, it is often found as ''krummholz'', trees growing close to the ground that have been dwarfed by exposure. In more favorable conditions, the trees may grow to in height. Identification Whitebark pine is a member of the Pinus classification, white pine group, the ''Pinus'' subgenus ''Strobus'', and the section ''Strobus''; like all members of this group, the leaves (needles) are in fascicle (botany), fascicles (bundles) of five with a decidu ...
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Abies Magnifica
''Abies magnifica'', the red fir or silvertip fir, is a western North American fir, native to the mountains of southwest Oregon and California in the United States. It is a high-elevation tree, typically occurring at elevation, though only rarely reaching tree line. The name red fir derives from the bark color of old trees. Description ''Abies magnifica'' is a large evergreen tree typically up to tall and trunk diameter, rarely to tall and diameter, with a narrow conic crown. The bark on young trees is smooth, grey, and has resin blisters, becoming orange-red, rough and fissured on old trees. The leaves are needle-like, long, glaucous blue-green above and below with strong stomatal bands, and an acute tip. They are arranged spirally on the shoot, but twisted slightly S-shaped to be upcurved above the shoot. The cones are erect, long, yellow-green (occasionally purple), ripening brown and disintegrating to release the winged seeds in fall. Varieties There are two, per ...
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Tsuga Mertensiana
''Tsuga mertensiana'', known as mountain hemlock, is a species of hemlock native to the west coast of North America, found between Southcentral Alaska and south-central California. Description ''Tsuga mertensiana'' is a large evergreen conifer growing up to tall, with exceptional specimens as tall as tall. They have a trunk diameter of up to . The bark is about thick and square-cracked or furrowed, and purplish-brown to gray in color. The crown is a neat, slender, conic shape in young trees with a tilted or drooping lead shoot, becoming cylindric in older trees. At all ages, it is distinguished by the slightly pendulous branchlet tips. The shoots are orange–brown, with dense pubescence about long. The leaves are needle-like, long and broad, soft, blunt-tipped, only slightly flattened in cross-section, pale glaucous blue-green above, and with two broad bands of bluish-white stomata below with only a narrow green midrib between the bands; they differ from those of any othe ...
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Hematite
Hematite (), also spelled as haematite, is a common iron oxide compound with the formula, Fe2O3 and is widely found in rocks and soils. Hematite crystals belong to the rhombohedral lattice system which is designated the alpha polymorph of . It has the same crystal structure as corundum () and ilmenite (). With this it forms a complete solid solution at temperatures above . Hematite naturally occurs in black to steel or silver-gray, brown to reddish-brown, or red colors. It is mined as an important ore mineral of iron. It is electrically conductive. Hematite varieties include ''kidney ore'', ''martite'' (pseudomorphs after magnetite), ''iron rose'' and ''specularite'' (specular hematite). While these forms vary, they all have a rust-red streak. Hematite is not only harder than pure iron, but also much more brittle. Maghemite is a polymorph of hematite (γ-) with the same chemical formula, but with a spinel structure like magnetite. Large deposits of hematite are found in ...
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