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Damon, Texas
Damon is a census-designated place (CDP) in Brazoria County, Texas, Brazoria County, Texas, United States. The population was 436 at the 2020 United States census, 2020 census. The town is located about south of Rosenberg, Texas, Rosenberg on Texas State Highway 36. Damon sits partly atop a salt dome which was exploited for petroleum, sulphur, and limestone. Geography Damon is located in northwestern Brazoria County at (29.289519, -95.737038). According to the United States Census Bureau, the CDP has a total area of , all land. Damon is from the San Bernard River and from the Brazos River. The community is between Needville, Texas, Needville in Fort Bend County and West Columbia, Texas, West Columbia in Brazoria County.211.pdf " Damon Independent School District. p. 1/5. Retrieved on December 5, 2016. Damon is home to the highest point in Brazoria ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Census-designated Place
A census-designated place (CDP) is a Place (United States Census Bureau), concentration of population defined by the United States Census Bureau for statistical purposes only. CDPs have been used in each decennial census since 1980 as the counterparts of incorporated places, such as self-governing city (United States), cities, town (United States), towns, and village (United States), villages, for the purposes of gathering and correlating statistical data. CDPs are populated areas that generally include one officially designated but currently unincorporated area, unincorporated community, for which the CDP is named, plus surrounding inhabited countryside of varying dimensions and, occasionally, other, smaller unincorporated communities as well. CDPs include small rural communities, Edge city, edge cities, colonia (United States), colonias located along the Mexico–United States border, and unincorporated resort and retirement community, retirement communities and their environs. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Texas State Highway 36
State Highway 36 (SH 36) runs from Freeport to Abilene. It was designated as the 36th Division Memorial Highway between Cameron and Sealy by the Texas Legislature in 1985. History SH 36 was originally proposed on November 21, 1917, as a route from Cisco to Waco. On December 20, 1917, this became part of SH 18. On November 20, 1917, an intercounty highway was designated from Goldthwaite to Temple. On January 24, 1918, the intercounty highway was extended to Cameron. On March 18, 1918, the intercounty highway was extended to Brenham. On March 20, 1918, SH 36 was designated as a route from Goldthwaite to Hearne. On January 23, 1919, SH 36 was extended to Richmond, and the old route had been changed to SH 36A. On March 19, 1919, SH 36 was extended to Freeport. On August 21, 1923, the sections from Temple to Goldthwaite and Richmond to Freeport were cancelled. On January 16, 1928, SH 36 was extended back to Freeport. On September 19, 1929, SH 36 was extended northwest to Ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anhydrite
Anhydrite, or anhydrous calcium sulfate, is a mineral with the chemical formula CaSO4. It is in the orthorhombic crystal system, with three directions of perfect cleavage parallel to the three planes of symmetry. It is not isomorphous with the orthorhombic barium (baryte) and strontium ( celestine) sulfates, as might be expected from the chemical formulas. Distinctly developed crystals are somewhat rare, the mineral usually presenting the form of cleavage masses. The Mohs hardness is 3.5, and the specific gravity is 2.9. The color is white, sometimes greyish, bluish, or purple. On the best developed of the three cleavages, the lustre is pearly; on other surfaces it is glassy. When exposed to water, anhydrite readily transforms to the more commonly occurring gypsum, (CaSO4·2H2O) by the absorption of water. This transformation is reversible, with gypsum or calcium sulfate hemihydrate forming anhydrite by heating to around under normal atmospheric conditions. Anhydrite is common ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gypsum
Gypsum is a soft sulfate mineral composed of calcium sulfate Hydrate, dihydrate, with the chemical formula . It is widely mined and is used as a fertilizer and as the main constituent in many forms of plaster, drywall and blackboard or sidewalk chalk. Gypsum also Crystallization, crystallizes as translucent crystals of selenite (mineral), selenite. It forms as an evaporite mineral and as a Mineral hydration, hydration product of anhydrite. The Mohs scale of mineral hardness defines gypsum as hardness value 2 based on Scratch hardness, scratch hardness comparison. Fine-grained white or lightly tinted forms of gypsum known as alabaster have been used for sculpture by many cultures including Ancient Egypt, Mesopotamia, Ancient Rome, the Byzantine Empire, and the Nottingham alabasters of Medieval England. Etymology and history The word ''wikt:gypsum, gypsum'' is derived from the Greek language, Greek word (), "plaster". Because the quarry, quarries of the Montmartre district of P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tertiary (period)
The Tertiary ( ) is an obsolete geologic period spanning 66 million to 2.6 or 1.8 million years ago. The period began with the extinction of the non- avian dinosaurs in the Cretaceous–Paleogene extinction event, at the start of the Cenozoic Era, and extended to the beginning of the Quaternary glaciation at the end of the Pliocene Epoch. The Tertiary has not been recognised by the International Commission on Stratigraphy (ICS) since the late 1980s, with the timespan of the Tertiary now being split in to the earlier Paleogene and the more recent Neogene periods, though the Tertiary continues to be used in some scientific publications. Historical use of the term The term Tertiary was first used by Giovanni Arduino during the mid-18th century. He classified geologic time into primitive (or primary), secondary, and tertiary periods based on observations of geology in Northern Italy. Later a fourth period, the Quaternary, was applied. In the early development of the study of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diapir
A diapir (; , ) is a type of intrusion in which a more mobile and ductilely deformable material is forced into brittle overlying rocks. Depending on the tectonic environment, diapirs can range from idealized mushroom-shaped Rayleigh–Taylor instability structures in regions with low tectonic stress such as in the Gulf of Mexico to narrow dikes of material that move along tectonically induced fractures in surrounding rock. The term was introduced by Romanian geologist Ludovic Mrazek, who was the first to understand the principle of salt tectonics and plasticity. The term ''diapir'' may be applied to '' igneous intrusions'', but it is more commonly applied to non-igneous, relatively cold materials, such as salt domes and mud diapirs. If a salt diapir reaches the surface, it can flow because salt becomes ductile with a small amount of moisture, forming a salt glacier. Occurrence Differential loading causes salt deposits covered by overburden (sediment) to rise upward tow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Damon Independent School District
Damon Independent School District is a public school district based in Damon, Texas (USA). The district covers grades Pre-Kindergarten through 8, making its school a K-8 school. History The date of establishment of the first school, located near an oil field, was not recorded; the 1900 Galveston hurricane destroyed this school. A replacement building opened shortly afterwards, and in 1921 a two-story building located between the current townsite and the former townsite opened. Damon High School opened in 1924. In 1947, Damon High School was closed.211.pdf " Damon Independent School District. p. 2/5. Retrieved on December 5, 2016. Damon ISD signed a contract with in 1949 so Damon ISD residents could go to school a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Columbia, Texas
West Columbia is a city in Brazoria County, Texas, United States. The city is centered on the intersection of Texas Highways 35 & 36, southwest of downtown Houston. The population was 3,644 at the 2020 census. The 1st Congress of the Republic of Texas was convened in West Columbia on October 3, 1836. (It was then named simply Columbia.) Geography West Columbia is located in western Brazoria County at (29.141513, –95.647016), about west of the Brazos River. Texas State Highway 35 leads east to Angleton, the county seat, and southwest to Bay City. Texas Highway 36 leads north to Rosenberg and southeast to Freeport on the Gulf of Mexico. According to the United States Census Bureau, West Columbia has a total area of , of which , or 0.67%, is water. Demographics As of the 2020 United States census, there were 3,644 people, 1,398 households, and 984 families residing in the city. As of the census of 2000, there were 4,255 people, 1,607 households, and 1,099 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fort Bend County
Fort Bend County is a county located in the U.S. state of Texas. The county was founded on December 29, 1837, and organized the next year. It is named for a blockhouse at a bend of the Brazos River. The community developed around the fort in early days. The county seat is Richmond. The largest city located entirely within the county borders is Sugar Land. The largest city by population in the county is Houston, but most of Houston's population is located in neighboring Harris County. Fort Bend County is included in the Houston– The Woodlands–Sugar Land metropolitan statistical area. As of the 2020 census, its population was 822,779, making it the state's eighth-most populous county, and was estimated to be 958,434 in 2024. In 2017, ''Forbes'' ranked it the fifth-fastest growing county in the United States. History Before European settlement, the area was inhabited by Karankawa Indians. Spanish colonists generally did not reach the area during their colonization, settli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Needville, Texas
Needville is a city in Fort Bend County, Texas, United States. It is within the metropolitan area. The population was 3,089 at the 2020 census. History August Schendel founded the town of Schendelville in 1891 that contained his house, a store and a cotton gin. In 1894, he applied for a post office using the name "Needmore" as a joke, since they always needed more of everything. Due to Needmore, Texas already existing, the post office amended the name to "Needville".Odintz, Mark. "Needville, TX." Handbook of Texas. Accessed April 18, 2018. By 1898, Schendel had officially platted a town and begun selling lots. A school had been constructed in 1897. By 1903, Needville had a school for white children with one teacher and 97 pupils, and one school for black children with one t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brazos River
The Brazos River ( , ), called the ''Río de los Brazos de Dios'' (translated as "The River of the Arms of God") by early Spanish explorers, is the 14th-longest river in the United States at from its headwater source at the head of Blackwater Draw, Roosevelt County, New Mexico to its mouth at the Gulf of Mexico with a drainage basin. The river is closely associated with Texas history, particularly the Austin settlement and Texas Revolution eras. Today major Texas institutions such as Texas Tech University, Baylor University, and Texas A&M University are located close to the river's basin, as are parts of metropolitan Houston. Geography The Brazos proper begins at the confluence of the Salt Fork and Double Mountain Fork, two tributaries of the Upper Brazos that rise on the high plains of the Llano Estacado, flowing southeast through the center of Texas. Another major tributary of the Upper Brazos is the Clear Fork Brazos River, which passes by Abilene and joins the mai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
San Bernard River
The San Bernard River is a river in Texas. Course San Bernard River flows from a spring near New Ulm, Texas to its mouth on the Gulf of Mexico, some to the southeast of the source. It passes through portions of Austin, Brazoria, Colorado, Fort Bend, Matagorda and Wharton counties. It passes alongside the Attwater Prairie Chicken National Wildlife Refuge, which shelters one of the last populations of the critically endangered Attwater's prairie-chicken, a ground-dwelling grouse of the coastal prairie ecosystem. The San Bernard River is one of a small number of rivers in Texas which empties directly into the Gulf. Its mouth was impeded in 2005 causing it to drain into the Gulf Intracoastal Waterway, but was later corrected. Shortly after being opened back up, the entrance silted in again, and remains so at this time. Watershed The San Bernard drains approximately 1,850 square miles (4800 km2) of land, and its basin area is home to approximately 87,000 people acc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
