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Hedge Creek Falls
Hedge Creek Falls is a waterfall on Hedge Creek, in the Shasta Cascade area in Dunsmuir, California. There is a small cave located behind the waterfall, allowing visitors to walk behind the cascading water. Shortly after the waterfall, hedge creek flows into the Sacramento River south of Mossbrae Falls. There is a viewing platform over the river, with a view of Mount Shasta. Access to the waterfall and viewing platform is via a short hiking trail. The trail starts at a small park off the Dunsmuir Ave/Siskiyou Ave exit on Interstate 5.SacramentoRiver.org "Hedge Creek Falls Trail" http://www.sacramentoriver.org/access_site.php?access_site_id=252 The waterfall is down Hedge Creek Falls Trail. The close proximity to Interstate 5, makes the waterfall a very popular stopping point for passing motorists. Geology and Hydrology Hedge Creek Falls is located on the southernmost tip of a pre-Pleistocene lava flow from Mount Shasta. Thousands of years of erosion, mostly from the freezing ...
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Hedge Creek Falls, Dec 2012
A hedge or hedgerow is a line of closely spaced shrubs and sometimes trees, planted and trained to form a barrier or to mark the boundary of an area, such as between neighbouring properties. Hedges that are used to separate a road from adjoining fields or one field from another, and are of sufficient age to incorporate larger trees, are known as hedgerows. Often they serve as windbreaks to improve conditions for the adjacent crops, as in bocage country. When clipped and maintained, hedges are also a simple form of topiary. A hedge often operates as, and sometimes is called, a "live fence". This may either consist of individual fence posts connected with wire or other fencing material, or it may be in the form of densely planted hedges without interconnecting wire. This is common in tropical areas where low-income farmers can demarcate properties and reduce maintenance of fence posts that otherwise deteriorate rapidly. Many other benefits can be obtained depending on the spec ...
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Basaltic
Basalt (; ) is an aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the surface of a rocky planet or moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of Venus, which cover ~80% of the surface, are basaltic; the lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flows that can spread over great areas before cooling and solidifying. Flood basalts are thick sequence ...
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Landforms Of Siskiyou County, California
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ...
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Black Bart (outlaw)
Charles E. Boles (b. 1829; d. after February 28, 1888), also known as Black Bart, was an American outlaw noted for the poetic messages he left behind after two of his robberies. Often called Charley by his friends, he was also known as Charles (or C.E.) Bolton. Considered a gentleman bandit with a reputation for style and sophistication, he was one of the most notorious stagecoach robbers to operate in and around Northern California and southern Oregon during the 1870s and 1880s. Early life Charles Boles was born in Norfolk, England, to John and Maria Boles (sometimes spelled Bolles). He was the third of ten children, having six brothers and three sisters. When he was two years old, his parents immigrated to Jefferson County, New York, where his father purchased a farm north of Plessis Village in the direction of Alexandria Bay. California Gold Rush In late 1849, Boles and his brothers David and James joined in the California Gold Rush, prospecting in the North Fork of the A ...
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Yosemite
Yosemite National Park ( ) is an American national park in California, surrounded on the southeast by Sierra National Forest and on the northwest by Stanislaus National Forest. The park is managed by the National Park Service and covers an area of and sits in four County, countiescentered in Tuolumne County, California, Tuolumne and Mariposa County, California, Mariposa, extending north and east to Mono County, California, Mono and south to Madera County, California, Madera County. Designated a World Heritage Site in 1984, Yosemite is internationally recognized for its granite cliffs, waterfalls, clear streams, Sequoiadendron giganteum, giant sequoia groves, lakes, mountains, meadows, glaciers, and Biodiversity, biological diversity. Almost 95 percent of the park is designated National Wilderness Preservation System, wilderness. Yosemite is one of the largest and least fragmented habitat blocks in the Sierra Nevada, and the park supports a diversity of plants and animals. The ...
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Bridalveil Fall
Bridalveil Fall is one of the most prominent waterfalls in the Yosemite Valley in California. The waterfall is in height and flows year round. Geology The glaciers that carved Yosemite Valley left many hanging valleys that spawned the waterfalls that pour into the valley. Most of the waterways that fed these falls carved the hanging valleys into steep cascades, however Bridalveil Creek still leaps into the valley from the edge of the precipice, although that edge has moved back into an alcove from the original edge of the valley. While Yosemite Falls seem to also fall into this category, the original course took the Yosemite Creek down a gorge to the west of its current location. The primary source of Bridalveil Fall is Ostrander Lake, some to the south. In a brisk wind, the falling water is often blown sideways, and when the flow is light, it may not reach the ground directly below. Because of this, the Ahwahneechee Native Americans called this waterfall "''Pohono''", whi ...
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Glaciers
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur only ...
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Aquifer
An aquifer is an underground layer of water-bearing, permeable rock, rock fractures, or unconsolidated materials (gravel, sand, or silt). Groundwater from aquifers can be extracted using a water well. Aquifers vary greatly in their characteristics. The study of water flow in aquifers and the characterization of aquifers is called hydrogeology. Related terms include aquitard, which is a bed of low permeability along an aquifer, and aquiclude (or ''aquifuge''), which is a solid, impermeable area underlying or overlying an aquifer, the pressure of which could create a confined aquifer. The classification of aquifers is as follows: Saturated versus unsaturated; aquifers versus aquitards; confined versus unconfined; isotropic versus anisotropic; porous, karst, or fractured; transboundary aquifer. Challenges for using groundwater include: overdrafting (extracting groundwater beyond the Dynamic equilibrium, equilibrium yield of the aquifer), groundwater-related subsidence of land, gro ...
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Lava Flows
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''labes'' ...
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Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ...
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Hedge Creek Falls
Hedge Creek Falls is a waterfall on Hedge Creek, in the Shasta Cascade area in Dunsmuir, California. There is a small cave located behind the waterfall, allowing visitors to walk behind the cascading water. Shortly after the waterfall, hedge creek flows into the Sacramento River south of Mossbrae Falls. There is a viewing platform over the river, with a view of Mount Shasta. Access to the waterfall and viewing platform is via a short hiking trail. The trail starts at a small park off the Dunsmuir Ave/Siskiyou Ave exit on Interstate 5.SacramentoRiver.org "Hedge Creek Falls Trail" http://www.sacramentoriver.org/access_site.php?access_site_id=252 The waterfall is down Hedge Creek Falls Trail. The close proximity to Interstate 5, makes the waterfall a very popular stopping point for passing motorists. Geology and Hydrology Hedge Creek Falls is located on the southernmost tip of a pre-Pleistocene lava flow from Mount Shasta. Thousands of years of erosion, mostly from the freezing ...
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Interstate 5
Interstate 5 (I-5) is the main north–south Interstate Highway on the West Coast of the United States, running largely parallel to the Pacific coast of the contiguous U.S. from Mexico to Canada. It travels through the states of California, Oregon, and Washington, serving several large cities on the U.S. West Coast, including San Diego, Los Angeles, Sacramento, Portland, and Seattle. It is the only continuous Interstate highway to touch both the Mexican and the Canadian borders. Upon crossing the Mexican border at its southern terminus, I-5 continues to Tijuana, Baja California, as Mexico Federal Highway 1 (Fed. 1). Upon crossing the Canadian border at its northern terminus, it continues to Vancouver as British Columbia Highway 99 (BC 99). I-5 was originally created in 1956 as part of the Interstate Highway System, but it was predated by several auto trails and highways built in the early 20th century. The Pacific Highway auto trail was built ...
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