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Duffy's Peak
Duffy's Peak is a small hill or butte near the Salt Fork Brazos River in Garza County, Texas. Duffy's Peak extends less than above the river, yet despite its small size, it served as an important landmark for early surveyors of the region and is said to be named for a member of the original survey team who died and was buried nearby in the late 1870s. Duffy's Peak is located in the rolling plains to the south and east of the Caprock Escarpment of the Llano Estacado. The soils of the area are moderately deep silt loams that support mesquite, yucca, Cactus, cacti, and grasses. The local terrain is eroded, cut by highly intermittent streams such as the Salt Fork Brazos River, and its tributaries, such as McDonald Creek and Lake Creek. These streams typically flow only during periods of heavy rainfall, when flash floods sweep through the area. The erosionally resistant sandstones of the peak's cap have protected underlying soils that have remained intact, while surrounding sedime ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salt Fork Brazos River
The Salt Fork Brazos River is a braided, highly intermittent stream about long, heading along the edge of the Llano Estacado about east-southeast of Lubbock, Texas. From its source, it flows generally east-southeastward to join the Double Mountain Fork to form the Brazos River about west-northwest of Haskell, Texas.United States Board on Geographical Names. 1964. Decisions on Geographical Names in the United States, Decision list no. 6402, United States Department of the Interior, Washington DC, p. 53. The Salt Fork stretches across portions of Crosby, Garza, Kent, and Stonewall counties of West Texas. Geography The Salt Fork Brazos River begins as a dry channel (draw) near the edge of the Llano Estacado in Crosby County, about southwest of the cotton gin in the small farming community of Cap Rock, Texas. From the edge of the Caprock Escarpment, the stream channel generally runs southeastward across southern Crosby County, passing to the east of Courthouse Mountain an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cactus
A cactus (, or less commonly, cactus) is a member of the plant family Cactaceae, a family comprising about 127 genera with some 1750 known species of the order Caryophyllales. The word ''cactus'' derives, through Latin, from the Ancient Greek word (''káktos''), a name originally used by Theophrastus for a spiny plant whose identity is now not certain. Cacti occur in a wide range of shapes and sizes. Although some species live in quite humid environments, most cacti live in habitats subject to at least some drought. Many live in extremely dry environments, even being found in the Atacama Desert, one of the driest places on Earth. Because of this, cacti show many adaptations to conserve water. For example, almost all cacti are succulents, meaning they have thickened, fleshy parts adapted to store water. Unlike many other succulents, the stem is the only part of most cacti where this vital process takes place. Most species of cacti have lost true leaves, retaining only spines, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of Texas
Texas contains a wide variety of geologic settings. The state's stratigraphy has been largely influenced by marine transgressive-regressive cycles during the Phanerozoic, with a lesser but still significant contribution from late Cenozoic tectonic activity, as well as the remnants of a Paleozoic mountain range. General geology Texas is approximately bisected by a series of faults that trend southwest to northeast across the state, from the area of Uvalde to Texarkana. South and east of these faults, the surface exposures consist mostly of Cenozoic sandstone and shale strata that grow progressively younger toward the coast, indicative of a regression that has continued from the late Mesozoic to the present. The coastal plain is underlaid by salt domes that are responsible for many of the oil traps in the region. North and west of the faults are the Stockton, Edwards, and Comanche plateaux; these define a crustal block that was upthrown during the Neogene. This large region of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mushaway Peak
Mushaway Peak is a small but conspicuous butte located southeast of Gail in central Borden County, Texas. It is one of the region's most venerable landmarks. The summit of this peak rises to an altitude of above sea level, which is roughly the same altitude as the High Plains of the Llano Estacado to the northwest. Mushaway Peak is in fact an erosional remnant of what was once a much larger Llano Estacado that has gradually retreated by the process of headward erosion. Its resistant cap has protected its underlying sediments, which have remained intact while surrounding sediments have been eroded away by Grape Creek and Bull Creek, two tributaries of the upper Colorado River. Proper name Mushaway Peak has been known by various names, including: Cordova Mountain, Cordova Peak, De Corde Peak, Mount Irwin, Mochaquo Mountain, Muchakooago Peak, Mucha Koo Ave, Mucha Kooay Mountain, Muchakooayo Peak, Muchakooay Peak, Mucha Koody Mountain, Mucha Kooga, Muchakooga Peak, Muchakooyo Pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Blanco
Mount Blanco is a small white hill — an erosional remnant — located on the eastern border of the Llano Estacado within Blanco Canyon in Crosby County, Texas. With Blanco Canyon, it is the type locality of the Blanco Formation of Texas and Kansas, as well as the Blancan fauna, which occurs throughout North America. Geology The term "Blanco Canyon beds", later shortened to "Blanco beds", was first applied to this formation in 1890 by William F. Cummins of the Geological Survey of Texas. The Blanco beds are considered to be of lacustrine origin – deposited in a Pleistocene lake basin set upon the Ogallala Formation of Pliocene age, which underlies the upper surface sediments of the Llano Estacado. The thickness of the Blanco beds varies from around thick. The formation mainly consists of light-gray, fine-grained mudstone, sandstone, and some conglomerate. These light-colored sediments contrast sharply with the locally rust-colored sediments of the Ogallala Formation. Fossi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Double Mountain Fork Brazos River
The Double Mountain Fork Brazos River is an ephemeral, sandy-braided stream about long, heading on the Llano Estacado of West Texas about southeast of Tahoka, Texas, flowing east-northeast across the western Rolling Plains to join the Salt Fork, forming the Brazos River about west-northwest of Haskell, Texas.United States Board on Geographical Names. 1964. Decisions on Geographical Names in the United States, Decision list no. 6402, United States Department of the Interior, Washington DC, p. 51. Geography The Double Mountain Fork Brazos River begins as a shallow draw near the eastern edge of the Llano Estacado in Lynn County, about northeast of the small farming community of Draw, Texas. The stream generally runs eastward across southern Garza County, where it is fed by springs, providing a minimal base flow that is intermittently punctuated by rainfall and associated runoff. At the western edge of Kent County, about east-northeast of Justiceburg, the Double Mountain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Texas State Highway 207
State Highway 207 (SH 207) is a state Highway that runs from Post, Texas through the South Plains and Texas Panhandle to the Texas/Oklahoma state line. History The highway was originally designated on July 31, 1934 between Floydada and Ralls. By 1939, the designation was extended north to Silverton and south to Garden City. On August 1, 1938, a section from Post to Garden City was designated, creating a gap. On October 24, 1938, the section from Ralls to Post was added, closing the gap. On February 21, 1939, SH 207 was extended north to Silverton. On August 27, 1940, the section of SH 207 from Big Spring to Garden City was cancelled. On February 4, 1941, the section of SH 207 from Gail to 8 miles north of Big Spring was cancelled. on March 6, 1941, the section of SH 207 from 8 miles north of Big Spring to Big Spring and the section of SH 207 from Post to Gail was cancelled. On February 28, 1945, the section of SH 207 from Ralls to Post was cancelled and transferred to FM 122. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Texas Historical Commission
The Texas Historical Commission is an agency dedicated to historic preservation within the state of Texas. It administers the National Register of Historic Places for sites in Texas. The commission also identifies Recorded Texas Historic Landmarks (RTHL) and recognizes them with Official Texas Historical Marker (OTHM) medallions and descriptive plaques. The commission identifies State Archeological Landmarks and Historic Texas Cemeteries. A quarterly publication, ''The Medallion,'' is published by the agency and includes news and advice about preservation projects, Texas’ historic sites, and heritage tourism opportunities. The agency also maintains the online Texas Historic Sites Atlas featuring more than 300,000 site records, including data on Official Texas Historical Markers and National Register of Historic Places properties in Texas. The commission has main offices in the Capitol Complex in downtown Austin; the complex includes the Carrington-Covert House, Luther Hal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grass
Poaceae () or Gramineae () is a large and nearly ubiquitous family of monocotyledonous flowering plants commonly known as grasses. It includes the cereal grasses, bamboos and the grasses of natural grassland and species cultivated in lawns and pasture. The latter are commonly referred to collectively as grass. With around 780 genera and around 12,000 species, the Poaceae is the fifth-largest plant family, following the Asteraceae, Orchidaceae, Fabaceae and Rubiaceae. The Poaceae are the most economically important plant family, providing staple foods from domesticated cereal crops such as maize, wheat, rice, barley, and millet as well as feed for meat-producing animals. They provide, through direct human consumption, just over one-half (51%) of all dietary energy; rice provides 20%, wheat supplies 20%, maize (corn) 5.5%, and other grains 6%. Some members of the Poaceae are used as building materials (bamboo, thatch, and straw); others can provide a source of biofuel, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yucca
''Yucca'' is a genus of perennial shrubs and trees in the family Asparagaceae, subfamily Agavoideae. Its 40–50 species are notable for their rosettes of evergreen, tough, sword-shaped leaves and large terminal panicles of white or whitish flowers. They are native to the hot and dry (arid) parts of the Americas and the Caribbean. Early reports of the species were confused with the cassava (''Manihot esculenta''). Consequently, Linnaeus mistakenly derived the generic name from the Taíno word for the latter, ''yuca''. The Aztecs living in Mexico since before the Spanish arrival, in Nahuatl, call the local yucca species (''Yucca gigantea'') , which gave the Spanish . is also used for ''Yucca filifera''. Distribution The natural distribution range of the genus ''Yucca'' (49 species and 24 subspecies) covers a vast area of the Americas. The genus is represented throughout Mexico and extends into Guatemala (''Yucca guatemalensis''). It also extends to the north through Baja Cali ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Texas
West Texas is a loosely defined region in the U.S. state of Texas, generally encompassing the arid and semiarid lands west of a line drawn between the cities of Wichita Falls, Abilene, and Del Rio. No consensus exists on the boundary between East Texas and West Texas. While most Texans understand these terms, no boundaries are officially recognized and any two individuals are likely to describe the boundaries of these regions differently. Walter Prescott Webb, American historian and geographer, suggested that the 98th meridian separates East and West Texas; Texas writer A.C. Greene proposed that West Texas extends west of the Brazos River. Use of a single line, though, seems to preclude the use of other separators, such as an area— Central Texas. Unlike East Texas, West Texas is not generally considered to be part of the American South, and the dry, desert climate is often more associated with the American Southwest. West Texas is often subdivided according to disti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesquite
Mesquite is a common name for several plants in the genus ''Prosopis'', which contains over 40 species of small leguminous trees. They are native to dry areas in the Americas. They have extremely long roots to seek water from very far under ground. As a legume, mesquites are one of the few sources of fixed nitrogen in the desert habitat. These trees bloom from spring to summer. They often produce fruits known as "pods". ''Prosopis'' spp. are able to grow up to tall, depending on site and climate. They are deciduous and depending on location and rainfall have either deep or shallow roots. ''Prosopis'' is considered long-lived because of the low mortality rate after the dicotyledonous stage and juveniles are also able to survive in conditions with low light and drought. The Cahuilla indigenous people of western North America were known to eat the seeds of mesquite. History ''Prosopis'' spp. have been in North America since the Pliocene era and their wood has been dated to 3300 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
