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Markagunt Plateau
Markagunt Plateau is a volcanic field in southern Utah, United States. Formed in a region of older volcanics, it consists of several cinder cones and associated lava flows. Some of the lava flows feature lava tubes such as Mammoth Cave, while others have formed lava dams and lakes like Navajo Lake. Volcanism took place during the Pliocene and latest Pleistocene but may have continued into the Holocene; legends of the Southern Paiute may reflect past eruptions. Geography and geomorphology The Markagunt Plateau is in southern Utah in the counties Iron County, Garfield County and Kane County. Cedar City lies west and Kanab south of the volcanic field, which is crossed by Utah State Route 14, Utah State Route 143 and Utah State Route 148. Towns in the area include Duck Creek Village and Mammoth Creek. The volcanic field is on a plateau bordered to the south by the Pink Cliffs and to the west by the cliffs of Cedar Breaks National Monument, and features lava flows and over 25 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Paiute People
The Southern Paiute people are a tribe of Native Americans who have lived in the Colorado River basin of southern Nevada, northern Arizona, and southern Utah. Bands of Southern Paiute live in scattered locations throughout this territory and have been granted federal recognition on several reservations. The first European contact with the Southern Paiute occurred in 1776, when fathers Silvestre Vélez de Escalante and Francisco Atanasio Domínguez encountered them during an attempt to find an overland route to the missions of California. They noted that some of the Southern Paiute men "had thick beards and were thought to look more in appearance like Spanish men than native Americans". Before this date, the Southern Paiute suffered slave raids by the Navajo and the Ute. The arrival of Spanish and later Euro-American explorers into their territory increased slave raiding by other tribes. In 1851, Mormon settlers strategically occupied Paiute water sources, which created a depen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kane County, Utah
Kane County is a county in the U.S. state of Utah. As of the 2010 United States Census, the population was 7,125. Its county seat and largest city is Kanab. History The county was created on January 16, 1864, by the Utah Territory legislature, with areas partitioned from Washington County. It was named for Col. Thomas L. Kane, a friend of the Latter Day Saint settlers in the 1840s and 1850s. The county boundary was adjusted in 1869, when a portion was returned to Washington County; in 1880, when San Juan County was created; and in 1883, when portions were partitioned from Kane and added to Iron and Washington counties. Geography Kane County lies on the south line of the state of Utah. Its south border abuts the northern border of the state of Arizona. The Colorado River, reformed as Lake Powell, forms its eastern border. Grand Staircase–Escalante National Monument covers much of the county. A rugged and inhospitable country of deserts, mountains, and cliffs make up the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A '' fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can bl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lineament
''See also Line (geometry)'' A lineament is a linear feature in a landscape which is an expression of an underlying geological structure such as a fault. Typically a lineament will appear as a fault-aligned valley, a series of fault or fold-aligned hills, a straight coastline or indeed a combination of these features. Fracture zones, shear zones and igneous intrusions such as dykes can also be expressed as geomorphic lineaments. Lineaments are often apparent in geological or topographic maps and can appear obvious on aerial or satellite photographs. There are for example, several instances within Great Britain. In Scotland the Great Glen Fault and Highland Boundary Fault give rise to lineaments as does the Malvern Line in western England and the Neath Disturbance in South Wales. The term 'megalineament' has been used to describe such features on a continental scale. The trace of the San Andreas Fault might be considered an example.Whitten & Brooks, The Penguin Dictionary of Geol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciation
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial peri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Panguitch
Panguitch ( ) is a city in and the county seat of Garfield County, Utah, United States. The population was 1,520 at the 2010 census, and was estimated in 2018 to be 1,691. The name Panguitch comes from a Southern Paiute word meaning “Big Fish,” likely named after the plentiful nearby lakes hosting rainbow trout year-round. Geography Panguitch is located on the western edge of Garfield County at (37.822234, -112.434650), in the valley of the Sevier River. U.S. Route 89 passes through the center of town, leading north to Junction and south to Orderville. Utah State Route 143 leads southwest from Panguitch to Panguitch Lake in Dixie National Forest. According to the United States Census Bureau, the city has a total area of , all land. Climate Panguitch has a cool semi-arid climate ( Köppen ''BSk'') with summers featuring hot afternoons and cold mornings, and cold, dry winters. The high altitude and relatively high latitude means that mornings are cold throughout the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Panguitch Lake
Panguitch Lake () was originally a large natural lake (777 acres) that has now been expanded by the creation of a dam to become a reservoir with a maximum surface area of . The lake, which drains into the Sevier River is located on the Markagunt Plateau, between Panguitch, Utah and Cedar Breaks National Monument. The lake is located in the Dixie National Forest in a high tourist use area near three national parks and one national monument. Panguitch Lake contains several campgrounds. Convenience stores and an LDS chapel are within walking distance of the campgrounds, and the roads are well paved and maintained. Road access to the lake is provided by Utah State Route 143, also known as the Brian Head-Panguitch Lake Scenic Byway or Utah's Patchwork Parkway. The earliest known use of Panguitch Lake was as a fishery by Paiute Indians (''Panguitch'' means "big fish" in the Paiute language). Panguitch Lake was treated with rotenone beginning May 1, 2006 to potentially eradicate an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cedar Breaks National Monument
Cedar Breaks National Monument is a U.S. National Monument located in the U.S. state of Utah near Cedar City. Cedar Breaks is a natural amphitheater, stretching across , with a depth of over . The elevation of the rim of the amphitheater is over above sea level. Rising above the rim is the prominent Brian Head, the peak of which lies a short distance outside of the National Monument boundary. The rock of the amphitheater is more eroded than, but otherwise similar to, formations at nearby Bryce Canyon National Park, Red Canyon in Dixie National Forest, and select areas of Cedar Mountain (SR-14). Because of its elevation, snow often makes parts of the park inaccessible to vehicles from October through May. Its rim visitor center is open from June through October. Several hundred thousand people visit the monument annually. The monument area is the headwaters of Mammoth Creek, a tributary of the Sevier River. Flora and fauna Wildlife can often be seen in this high altitud ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliff
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs als ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Duck Creek Village, Utah
Duck Creek Village is an unincorporated community in Kane County, Utah, United States. Description The community is located on the edge of Cedar Mountain, with an elevation of . Duck Creek Village has a post office with the ZIP code of 84762. See also References External links * Unincorporated communities in Kane County, Utah Unincorporated communities in Utah {{Utah-geo-stub ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Utah State Route 148
State Route 148 (SR-148) is a state highway in the U.S. state of Utah. The entire highway has been designated the Cedar Breaks Scenic Byway as part of the Utah Scenic Byways and National Forest Scenic Byway programs. Route description The route starts at its intersection with State Route 14 in Cedar Canyon. From here it travels north approximately north to its terminus at the south boundary of Cedar Breaks National Monument. While the route ends here, continuing north along the road into the park leads to Utah's Patchwork Parkway/Brian Head-Lake Panguitch Scenic Byway (SR-143). History State Route 55 was designated by the Utah State Legislature in 1927, connecting SR-14 at Cedar Breaks Junction with the southern boundary of Cedar Breaks National Monument. However, as part of a major realignment of state highways, SR-55 was deleted in 1969, and the route was designated as part of SR-143. This left SR-143 as a non-contiguous highway, as the portion going through the nati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Utah State Route 143
State Route 143 (SR-143) is a state highway in the U.S. state of Utah. The entire highway has been designated the Brian Head-Panguitch Lake Scenic Byway as part of the Utah Scenic Byways program. This road has also been designated as Utah's Patchwork Parkway as part of the National Forest Scenic Byway and National Scenic Byway programs. At just over long, it connects Parowan to Panguitch while providing access to Brian Head, Cedar Breaks National Monument, and Panguitch Lake. It is also the second-highest paved road in the state at above sea level. The western section of the road from Parowan started as a logging road for nineteenth century Mormon pioneers and was designated a state highway in 1933. Twenty years later, the route was extended to Cedar Breaks National Monument, and again in 1985 to its present-day eastern end in Panguitch. Route description State Route 143 begins at Interstate 15 in Iron County just west of Parowan as 200 South and travels through the ce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Markagunt Plateau")
