Kalgary, Texas
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Kalgary, Texas
Kalgary is an unincorporated community in Crosby County, Texas, United States. According to the ''Handbook of Texas'', the community had an estimated population of 70 in 2000. Kalgary is part of the Lubbock Metropolitan Statistical Area. Geography Kalgary is situated along FM 261 in southeastern Crosby County, about southeast of Lubbock. It is located within the rolling plains along a drainage divide that separates the White River and the Salt Fork Brazos River, both tributaries of the Brazos River. Climate According to the Köppen climate classification system, Kalgary has a semiarid climate, ''BSk'' on climate maps. History The community was established around 1905, when E.P. Swenson started selling parcels of his SMS Ranch. First known as Spur, the community became known as Watson, after early settler Richard Watson Self. A post office opened in 1911, but closed two years later. It reopened in 1925, and in 1927, the community's name was changed from Watson to Kalgary after ...
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Unincorporated Community
An unincorporated area is a region that is not governed by a local municipal corporation. Widespread unincorporated communities and areas are a distinguishing feature of the United States and Canada. Most other countries of the world either have no unincorporated areas at all or these are very rare: typically remote, outlying, sparsely populated or uninhabited areas. By country Argentina In Argentina, the provinces of Chubut, Córdoba, Entre Ríos, Formosa, Neuquén, Río Negro, San Luis, Santa Cruz, Santiago del Estero, Tierra del Fuego, and Tucumán have areas that are outside any municipality or commune. Australia Unlike many other countries, Australia has only one level of local government immediately beneath state and territorial governments. A local government area (LGA) often contains several towns and even entire metropolitan areas. Thus, aside from very sparsely populated areas and a few other special cases, almost all of Australia is part of an LGA. Uninc ...
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Farm To Market Road 261
A farm (also called an agricultural holding) is an area of land that is devoted primarily to agricultural processes with the primary objective of producing food and other crops; it is the basic facility in food production. The name is used for specialized units such as arable farms, vegetable farms, fruit farms, dairy, pig and poultry farms, and land used for the production of natural fiber, biofuel and other commodities. It includes ranches, feedlots, orchards, plantations and estates, smallholdings and hobby farms, and includes the farmhouse and agricultural buildings as well as the land. In modern times the term has been extended so as to include such industrial operations as wind farms and fish farms, both of which can operate on land or sea. There are about 570 million farms in the world, most of which are small and family-operated. Small farms with a land area of fewer than 2 hectares operate about 1% of the world's agricultural land, and family farms comprise about 75 ...
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McDonald Creek (Salt Fork Brazos River Tributary)
McDonald Creek is an intermittent stream, about long, heading about south-southwest of Crosbyton, Texas, and trending generally southeast to join the Salt Fork Brazos River near the community of Verbena, Texas. Geography McDonald Creek rises along the eastern edge of the Caprock Escarpment of the Llano Estacado. The stream channel initially runs southeast then curves to the southwest where it merges with Turkey Creek about west-northwest of Kalgary, Texas. It then runs south to join Lake Creek about upstream of Farm to Market Road 651. The stream then runs southeast where it merges with the Salt Fork Brazos River at a low-water crossing on Farm to Market Road 2008, near the sparsely populated community of Verbena. Overall, McDonald Creek descends about from its source to its mouth, passing through highly eroded and moderately steep terrain along its course. See also *List of rivers of Texas *Caprock Escarpment *Canyon Valley, Texas *Double Mountains (Texas) *Duffy's Peak ...
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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 ...
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Estacado, Texas
Estacado is a ghost town in Crosby and Lubbock Counties in the U.S. state of Texas. Located along Farm to Market Road 1527, it was established in 1879 as a Religious Society of Friends (Quaker) colony by Paris Cox and originally named Maryetta after his wife. In 1886, it became the first government seat of Crosby County. In 1936, Recorded Texas Historic Landmark number 4779 was designated to commemorate the founding of Estacado. Paris Cox Paris Cox (1846–1888) was born one of six children in a devout Religious Society of Friends family near Asheboro, North Carolina. During the Civil War, Cox was given a legal exemption from military service, based on the Quaker precept of pacifism. As treasurer of the North Carolina fellowship of Quakers, Cox was instrumental in helping the Religious Society of Friends, known as Quakers, find a favorable location for both farming and freedom from religious persecution. Their first move from North Carolina was to Indiana. Cox married Mary C. Fe ...
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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 ...
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Canyon Valley, Texas
Canyon Valley is a ghost town in southern Crosby County, Texas, United States. Today, only a few farms and ranches are scattered across the area. Geography Canyon Valley is located south of Ralls in southwestern Crosby County. Only one road passes through Canyon Valley, and it is unpaved and passes through a low-water crossing that is often impassable during wet weather. The nearest paved road is Texas State Highway 207, which passes to the west at a distance around . Canyon Valley lies below the Caprock, which defines the southeastern edge of the vast Llano Estacado. It lies within the physiographic region known as the Rolling Plains in the highly eroded valley of the Salt Fork Brazos River. History In 1925, James A. Shoemaker brought his family to Crosby County, where he bought a quarter-section of land 3 miles south of the small community of Cap Rock. A three-room house was built on the property, while the land was cleared for farming. Water was hauled in barrels by w ...
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Crosbyton Consolidated Independent School District
Crosbyton Consolidated Independent School District is a public school district based in Crosbyton, Texas, United States. It is located in Crosby County, a small portion of the district extends into Garza County. Crosbyton Consolidated ISD has three campuses – Crosbyton High (grades 9–12), Crosbyton Middle (grades 6–8), and Crosbyton Elementary (grades PK–5). On July 1, 1985, portions of the McAdoo Independent School District were incorporated into Crosbyton ISD. The new entity was renamed to the Crosbyton Consolidated Independent School District. In 2009, the school district was rated " academically acceptable" by the Texas Education Agency The Texas Education Agency (TEA) is the branch of the government of Texas responsible for public education in Texas in the United States.
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Crosbyton, Texas
Crosbyton is a city in and the county seat of Crosby County, Texas, United States. The population was 1,741 at the 2010 census. Crosbyton is part of the Lubbock Metropolitan Statistical Area. History The city was named for land office commissioner Stephen Crosby. Geography Crosbyton is located slightly northeast of the center of Crosby County at (33.656733, –101.238811), along U.S. Route 82 about west of Blanco Canyon at the eastern edge of the Llano Estacado. US 82 leads east to Dickens and west to Lubbock. According to the United States Census Bureau, Crosbyton has a total area of , all of it land. Demographics 2020 census As of the 2020 United States census, there were 1,492 people, 667 households, and 498 families residing in the city. 2000 census As of the census of 2000, 1,874 people, 677 households, and 482 families resided in the city. The population density was 886.9 people per square mile (342.9/km). The 781 housing units averaged 369.6 per square m ...
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Calgary
Calgary ( ) is the largest city in the western Canadian province of Alberta and the largest metro area of the three Prairie Provinces. As of 2021, the city proper had a population of 1,306,784 and a metropolitan population of 1,481,806, making it the third-largest city and fifth-largest metropolitan area in Canada. Calgary is situated at the confluence of the Bow River and the Elbow River in the south of the province, in the transitional area between the Rocky Mountain Foothills and the Canadian Prairies, about east of the front ranges of the Canadian Rockies, roughly south of the provincial capital of Edmonton and approximately north of the Canada–United States border. The city anchors the south end of the Statistics Canada-defined urban area, the Calgary–Edmonton Corridor. Calgary's economy includes activity in the energy, financial services, film and television, transportation and logistics, technology, manufacturing, aerospace, health and wellness, retail, and ...
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Semiarid Climate
A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes. Defining attributes of semi-arid climates A more precise definition is given by the Köppen climate classification, which treats steppe climates (''BSk'' and ''BSh'') as intermediates between desert climates (BW) and humid climates (A, C, D) in ecological characteristics and agricultural potential. Semi-arid climates tend to support short, thorny or scrubby vegetation and are usually dominated by either grasses or shrubs as it usually can't support forests. To determine if a location has a semi-arid climate, the precipitation threshold must first be determined. The method used to find the precipitation threshold (in millimeters): *multiply by ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ...
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