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Ranger Oil Boom
The Ranger Oil Boom started on October 17, 1917, after oil was discovered at the ''J.H. McCleskey No. 1'' drill well when oil roared up from below ground in Ranger, Texas. The strike was notable because the threatened exit of Soviet Russia from World War I meant a lot of oil output was lost to the Allies. Before WWI Russia accounted for 30% of the world's oil production, more than any other country. On December 15, 1917, an armistice between Soviet Russia and the Central Powers was concluded. According to a story from USA Today, the oil from the Ranger Oil Strike helped win World War I. Discovery William Knox Gordon made his fortune with the Texas and Pacific Coal Company in Thurber, Texas, no relation to the Texas and Pacific Railway although they did business. He saw the writing on the wall and wanted to diversify into the oil and petroleum industry. William Gordon and his Texas Pacific Coal Company of Thurber, Texas, drilled a gas well north of Ranger in August 1917, af ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ranger, Texas
Ranger is a city in Eastland County, Texas, United States. Its population was 2,468 at the 2010 census. Ranger College, a community college, is the second-largest employer in the community. During the 1920s, Ranger, like nearby Cisco, Eastland, and Desdemona, was a petroleum boomtown. History The Texas Pacific Coal Company of Thurber, Texas, drilled a gas well north of Ranger in August 1917, after town civic leaders offered acreage in return for four test wells. Then on 11 October 1917, the McClesky well, 1 mile southwest of Ranger, produced oil at 1200 BOPD. Production came from the Strawn Formation sandstones at , the Smithwick Shale, and the Marble Falls Formation limestone at feet. The Ranger Oil Field production peaked in July 1919 at 80,000 BOPD. The oil boom brought many seeking jobs, including farm boys and demobilized veterans. Geography Ranger is located in northeastern Eastland County at (32.470102, –98.676734). Interstate 20 passes south and east of the ci ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Treaty Of Brest-Litovsk
The Treaty of Brest-Litovsk (also known as the Treaty of Brest in Russia) was a separate peace, separate peace treaty signed on 3 March 1918 between Russian SFSR, Russia and the Central Powers (German Empire, Germany, Austria-Hungary, Kingdom of Bulgaria, Bulgaria, and the Ottoman Empire), that ended Eastern Front (World War I), Russia's participation in World War I. The treaty was signed at German-controlled Brest-Litovsk ( pl, Brześć Litewski; since 1945, Brest, Belarus, Brest, now in modern Belarus), after two months of negotiations. The treaty was agreed upon by the Russians to stop further invasion. As a result of the treaty, Soviet Russia defaulted on all of Imperial Russia's commitments to the Allies of World War I, Allies and eleven nations became independent in eastern Europe and western Asia. Under the treaty, Russia lost all of Ukrainian People's Republic, Ukraine and most of Belarusian People's Republic, Belarus, as well as its three Baltic states, Baltic republics of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
World War I
World War I (28 July 1914 11 November 1918), often abbreviated as WWI, was one of the deadliest global conflicts in history. Belligerents included much of Europe, the Russian Empire, the United States, and the Ottoman Empire, with fighting occurring throughout Europe, the Middle East, Africa, the Pacific, and parts of Asia. An estimated 9 million soldiers were killed in combat, plus another 23 million wounded, while 5 million civilians died as a result of military action, hunger, and disease. Millions more died in genocides within the Ottoman Empire and in the 1918 influenza pandemic, which was exacerbated by the movement of combatants during the war. Prior to 1914, the European great powers were divided between the Triple Entente (comprising France, Russia, and Britain) and the Triple Alliance (containing Germany, Austria-Hungary, and Italy). Tensions in the Balkans came to a head on 28 June 1914, following the assassination of Archduke Franz Ferdin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Armistice Between Russia And The Central Powers
On , an armistice was signed between the Russian Soviet Federative Socialist Republic on the one side and the Austro-Hungarian Empire, the Kingdom of Bulgaria, the German Empire and the Ottoman Empire—the Central Powers—on the other. The armistice took effect two days later, on . By this agreement Russia ''de facto'' exited World War I, although fighting would briefly resume before the Treaty of Brest-Litovsk was signed on 3 March 1918, and Russia made peace. Ceasefires The Bolsheviks came to power with the slogan "Bread and Peace". On three Russian emissaries under a white flag entered the German lines to arrange for negotiations which they agreed would be held at the headquarters of the Central Powers Armies at Brest-Litovsk. A local ceasefire agreement was reached at Soly on between the Russians and Germans on the Eastern Front (Russia's "Western Front"). It superseded any local ceasefires or truces already agreed to—without specifying what these were—and was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thurber, Texas
Thurber is an unincorporated community in Erath County, Texas, United States (near the Palo Pinto county line), located 75 miles west of Fort Worth. It was, between 1888 and 1921, one of the largest producers of bituminous coal in Texas and the largest company town in the state, with a population of over 10,000. The population of the community is 48 per the 2010 United States Census. History Coal-mining operations began in Thurber in 1886 and reached a peak around 1920, when the town had a population of approximately 8,000 to 10,000, from more than a dozen nationalities, though Italians, Poles, and Mexicans predominated. At the peak, Thurber was one of the largest bituminous coal-mining towns in Texas. Established as a company town, the mining operations in Thurber were unionized in 1903 and Thurber became the first totally closed shop town in the country. The Texas and Pacific Coal Company was not owned by the Texas and Pacific Railway, but it lay near its line and pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Texas And Pacific Railway
The Texas and Pacific Railway Company (known as the T&P) was created by federal charter in 1871 with the purpose of building a southern transcontinental railroad between Marshall, Texas, and San Diego, California. History Under the influence of General Buell the TPRR was originally to be gauge, but this was overturned when the state legislature passed a law requiring gauge. The T&P had a significant foothold in Texas by the mid-1870s. Construction difficulties delayed westward progress, until American financier Jay Gould acquired an interest in the railroad in 1879. The T&P never reached San Diego; instead it met the Southern Pacific at Sierra Blanca, Texas, in 1881. The Missouri Pacific Railroad, also controlled by Gould, leased the T&P from 1881 to 1885 and continued a cooperative relationship with the T&P after the lease ended. Missouri Pacific gained majority ownership of the Texas and Pacific Railway's stock in 1928 but allowed it to continue operation as a separate en ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
BOPD
A barrel is one of several units of volume applied in various contexts; there are dry barrels, fluid barrels (such as the U.K. beer barrel and U.S. beer barrel), oil barrels, and so forth. For historical reasons the volumes of some barrel units are roughly double the volumes of others; volumes in common use range approximately from . In many connections the term is used almost interchangeably with ''barrel''. Since medieval times the term as a unit of measure has had various meanings throughout Europe, ranging from about 100 litres to about 1,000 litres. The name was derived in medieval times from the French , of unknown origin, but still in use, both in French and as derivations in many other languages such as Italian, Polish, and Spanish. In most countries such usage is obsolescent, increasingly superseded by SI units. As a result, the meaning of corresponding words and related concepts (vat, cask, keg etc.) in other languages often refers to a physical container ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Strawn Formation
The Strawn Formation is a geologic formation in Texas. It preserves fossils dating back to the Carboniferous period. See also * List of fossiliferous stratigraphic units in Texas * Paleontology in Texas Paleontology in Texas refers to paleontological research occurring within or conducted by people from the U.S. state of Texas. Author Marian Murray has remarked that "Texas is as big for fossils as it is for everything else." Some of the most impor ... References * Carboniferous Texas {{Carboniferous-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marble Falls Formation
The Marble Falls Formation is a geologic formation in Texas. It preserves fossils dating back to the Carboniferous period. See also * List of fossiliferous stratigraphic units in Texas * Paleontology in Texas Paleontology in Texas refers to paleontological research occurring within or conducted by people from the U.S. state of Texas. Author Marian Murray has remarked that "Texas is as big for fossils as it is for everything else." Some of the most impor ... References * Carboniferous Texas Carboniferous southern paleotropical deposits {{Carboniferous-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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