Bashi Creek
Bashi Creek, also historically known as Bashai Creek, is a tributary of the Tombigbee River in northern Clarke County in Alabama. Location Bashi Creek originates near Bashi, at coordinates of , and discharges into the Tombigbee River near Woods Bluff, at coordinates of . It is located above the Coffeeville Lock and Dam and is the only inlet off the river for several miles. There is a paved boat ramp located on the creek. Etymology The creek first appears on an 1844 map as Bashai Creek. Language scholars believe Bashi to be an adaptation of the Choctaw language word ''bachaya'', meaning "line," "row," or "course". Bashi Formation The creek has lent its name to the Bashi Formation, formerly also known as the Woods Bluff Formation, a greensand marl strata dating to the early Eocene. The creek flows through the exposed strata of the formation. Bashi Skirmish The Bashi Skirmish in the Creek War The Creek War (1813–1814), also known as the Red Stick War and the Creek C ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bashi, Alabama
Bashi is an unincorporated community in Clarke County, Alabama, United States. It takes its name from the nearby Bashi Creek that flows westward into the Tombigbee River The Tombigbee River is a tributary of the Mobile River, approximately 200 mi (325 km) long, in the U.S. states of Mississippi and Alabama. Together with the Alabama, it merges to form the short Mobile River before the latter empties int .... Geography Bashi is located at at an elevation of . Bashi is in the Central Time Zone. References Alabama placenames of Native American origin Unincorporated communities in Alabama Unincorporated communities in Clarke County, Alabama {{ClarkeCountyAL-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Marl
Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part of the cliffs of Dover, and the Channel Tunnel follows these marl layers between France and the United Kingdom. Marl is also a common sediment in post-glacial lakes, such as the marl ponds of the northeastern United States. Marl has been used as a soil conditioner and neutralizing agent for acid soil and in the manufacture of cement. Description Marl or marlstone is a carbonate-rich mud or mudstone which contains variable amounts of clays and silt. The term was originally loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwater conditions. These typically contain 35–65% clay and 65–35% carbonate. The te ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Tributaries Of The Tombigbee River
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & Scott ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Rivers Of Alabama
This is a list of rivers of the US state of Alabama. Alabama has over 77,000 miles of rivers and streams with more freshwater biodiversity than any other US state. Alabama's rivers are among the most biologically diverse waterways in the world. 38% of North America's fish species, 43% of its freshwater gill-breathing snails, 51% of its freshwater turtle species, and 60% of its freshwater mussel species are native to Alabama's rivers. List by drainage basin All rivers in Alabama eventually flow into the Gulf of Mexico. This list arranges rivers into drainage basin, which are ordered by the location of the mouth of the main stem from east to west. Tributaries are ordered from mouth to source (subject to being within the borders of Alabama). Gulf Coast (east) *''Apalachicola River (FL)'' **Chattahoochee River *** Cedar Creek *** Omusee Creek *** Abbie Creek **** Sandy Creek *** Cheneyhatchee Creek *** Barbour Creek *** Chewalla Creek *** Cowikee Creek **** North Fork Cowikee Cre ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Chicago, Illinois
(''City in a Garden''); I Will , image_map = , map_caption = Interactive Map of Chicago , coordinates = , coordinates_footnotes = , subdivision_type = Country , subdivision_name = United States , subdivision_type1 = State , subdivision_type2 = Counties , subdivision_name1 = Illinois , subdivision_name2 = Cook and DuPage , established_title = Settled , established_date = , established_title2 = Incorporated (city) , established_date2 = , founder = Jean Baptiste Point du Sable , government_type = Mayor–council , governing_body = Chicago City Council , leader_title = Mayor , leader_name = Lori Lightfoot ( D) , leader_title1 = City Clerk , leader_name1 = Anna Valencia ( D) , unit_pref = Imperial , area_footnotes = , area_tot ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Creek War
The Creek War (1813–1814), also known as the Red Stick War and the Creek Civil War, was a regional war between opposing Indigenous American Creek factions, European empires and the United States, taking place largely in modern-day Alabama and along the Gulf Coast. The major conflicts of the war took place between state militia units and the "Red Stick" Creeks. The United States government formed an alliance with the Choctaw Nation and Cherokee Nation (the traditional enemies of the Creeks), along with the remaining Creeks to put the rebellion down. According to historian John K. Mahon, the Creek War "was as much a civil war among Creeks as between red and white, and it pointed up the separation of Creeks and Seminoles". The war was also part of the centuries-long American Indian Wars. It is usually considered part of the War of 1812 because it was influenced by Tecumseh's War in the Old Northwest, was concurrent with the American-British portion of the war and involved m ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bashi Skirmish
The Bashi Skirmish in the Creek War was fought in what became Failetown, Alabama. A Clarke County historical marker which stands on Woods Bluff Road between Alabama 69 and Cassidy Hill marks the location of the incident which resulted in the death of 4 Americans. The exact date of this skirmish is not clear but it is believed to have occurred in early October 1813. At least one source puts it at October 4, 1813. A group of 25 white horsemen led by Colonel William McGrew left St. Stephens traveling towards Fort Easley. The company was proceeding towards a stream called Bashi Creek that flows into the Tombigbee River a mile or two north of Wood's Bluff when they suddenly found themselves among concealed Creek warriors. They were ambushed after a turkey tail was raised above a log by one of the concealed Creek, giving the signal for attack. The Indians who had guns instantly fired from their places of concealment and McGrew who had taken part in the Battle of Burnt Corn The ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope Carbon-13, 13C in the atmosphere was exceptionally low in comparison with the more common isotope Carbon-12, 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Popigai impact structure, Siberia and in what is now ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Greensand (geology)
Greensand or green sand is a sand or sandstone which has a greenish color. This term is specifically applied to shallow marine sediment that contains noticeable quantities of rounded greenish grains. These grains are called ''glauconies'' and consist of a mixture of mixed-layer clay minerals, such as smectite and glauconite. Greensand is also loosely applied to any glauconitic sediment. Formation Greensand forms in anoxic marine environments that are rich in organic detritus and low in sedimentary input. Having accumulated in marine environments, greensands can be fossil-rich, such as in the late-Cretaceous deposits of New Jersey. Occurrence Important exposures are known from both northern and western Europe, North America, southeastern Brazil and north Africa. Well known and important greensands are the Upper and Lower Greensands of England and occur within Eocene and Cretaceous sedimentary strata underlying the coastal plains of New Jersey and Delaware. Although greensand has ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Clarke County, Alabama
Clarke County is a county located in the southwestern part of the U.S. state of Alabama. As of the 2020 census, the population was 23,087. The county seat is Grove Hill. The county's largest city is Jackson. The county was created by the legislature of the Mississippi Territory in 1812. It is named in honor of General John Clarke of Georgia, who was later elected governor of that state. The county museum is housed in the Alston-Cobb House in Grove Hill. History Pre-European era For thousands of years, this area was occupied along the rivers by varying cultures of indigenous peoples. At the time of European encounter, Clarke County was the traditional home of the Choctaw and the Creek people. They traded with the French, who had settlements in Mobile and New Orleans. They also were reached by some English and Scots traders from the British colonies along the Atlantic Coast. After the Louisiana Purchase, they started to establish relations with the United States. In 180 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bashi Formation
The Bashi Formation is a geologic formation in Alabama and Mississippi. It is named for Bashi Creek in northern Clarke County, Alabama, which cuts through some of its exposures. It preserves fossils dating back to the Eocene period, or Wasatchian in the NALMA classification.Bashi Formation at .org Fossil content The following fossils have been reported from the formation: ;Reptiles * '' Palaeophis cf. littoralis''Parmley & Case, 1988 * ''[...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Choctaw Language
The Choctaw language (Choctaw: ), spoken by the Choctaw, an Indigenous people of the Southeastern Woodlands, is part of the Muskogean language family. Chickasaw is separate but closely related language to Choctaw. The Choctaw Nation of Oklahoma published the ''New Choctaw dictionary'' in 2016. Orthography The written Choctaw language is based upon the English version of the Roman alphabet and was developed in conjunction with the "civilization program" of the United States, a program to westernize and forcefully assimilate Indigenous Americans, particularly those adhering to what were to become the Five Civilized Tribes (of which the Choctaw are a part) into Anglo-American Culture and Sympathies during the early 19th century. Although there are other variations of the Choctaw alphabet, the three most commonly seen are the Byington (Traditional), Byington/Swanton (Linguistic), and Modern (Mississippi Choctaw). Many publications by linguists about the Choctaw language use a ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |