NoeFlandre/osm-polygon-wikidata-only huggingface dataset:
Mall of Abilene

Mall of Abilene is an enclosed shopping mall in Abilene, Texas. It is located in the south side of the city, at the southwest corner of Buffalo Gap Road and US 83/84 (Winters Freeway). Occupying a 61-acre plot of land, It serves a 22-county trade area. Five stores anchor the mall JCPenney, Dillard's, Best Buy, Ulta, and Books-A-Million with one vacant anchor last occupied by Sears. The mall also houses the 15,000 sq ft (1,400 m2) Premiere Cinema 10 in a converted UA Theaters 6. The mall's gross leasable area of nearly 1,000,000 sq ft (93,000 m2) consists of a total of 80 stores, excluding the theater, 7 of which have a leasable area of at least 56,000 sq ft (5,200 m2). As of 2005, the mall generates 8.7 million visitors per year. History The Mall of Abilene began its development in 1977, when ground was broken for a new shopping complex in the growing southern reaches of Abilene. Developed by Paul Broadhead & Associates, the complex would initially cost $28 million to develop, with the mall opening to shoppers in March 1979. The mall would open with Dillard's, JCPenney, Sears, H. J. Wilson Co. (later Service Merchandise, now the second Dillard's store) and Grissom's (later Dunlap's, now Best Buy, Books-a-Million, and Ulta) as its anchor stores. The mall's initial junior anchors would be Beall's, UA Theaters 6, Lerner's and Luby's Cafeteria. Some original inline tenants would include; Chick-fil-A (now closed), Express (now closed), GNC, El Chico, Footaction, Motherhood Maternity (now closed), Spencer's and Zales; all of which have been at the mall for the last 40 years. As the years progressed the makeup of these tenants had partially changed, at one point Grissom's was replaced by Dunlaps. Wilson's would re-open as Service Merchandise in 1985. Later on, tenants like Ulta Beauty and Chuck-E-Cheese would occupy the two spaces next to the main entrance, with the vacant Luby's becoming Ulta Beauty. On December 28, 2018, it was announced that Sears would be closing as part of a plan to close 80 stores nationwide. The store closed in March 2019. Tenants Anchors Source: Books-A-Million - 16,000 s.f. Best Buy - 24,000 s.f. Dillard's North (Men's) - 63,404 s.f. JCPenney - 96,108 s.f. Dillard's South (Women's) - 98,828 s.f. Sears - 142,604 s.f. [Vacant] Specialty Stores Source: Aeropostale American Eagle Outfitters JD Sports Hibbett Sports Space Golf Hot Topic LensCrafters Shoe Dept. Spencer Gifts Victoria's Secret Restaurants Source: Chuck E. Cheese Coastal Cookies Dante's Dippin Dots El Chico Joe Muggs (inside Books-A-Million) Cinemas Premiere Cinema 10 References External links Mall of Abilene
Odessa-Meteor-Krater

Die Odessa-Meteor-Krater sind Impaktkrater im Südwesten der Stadt Odessa, Ector County, Texas, USA. Fünf Krater sind identifiziert, wovon der größte fast 170 Meter Durchmesser hat. Der Hauptkrater war einer der ersten erkannten und untersuchten Impaktkrater. Im Umfeld der Krater wurden im Laufe der Jahre über 1500 Meteoritenbruchstücke gefunden. Sie gehören zu den Oktaedriten, einer Gruppe von Nickel-Eisenmeteoriten. Das größte Stück wog ungefähr 135 Kilogramm. Bei Ausgrabungen im Hauptkrater konnte keine größere Meteoritenmasse gefunden werden. Es wird angenommen, dass es dort niemals einen großen Meteoriten gab. Die Einschlagsereignisse fanden vor höchstens 63.500 Jahren statt, wobei der ursprünglich 30 Meter tiefe Hauptkrater heute noch etwa 5 Meter tief ist. Er ist als nationales Naturdenkmal ausgewiesen und mit einem Informationszentrum (dem Odessa Meteor Crater Museum) und Lehrpfad ausgestattet. Siehe auch Liste der Einschlagkrater der Erde Quellen Odessa (iron). In: Meteoritical Bulletin Database;. Abgerufen am 30. Januar 2021. TSHA – Meteor Crater At Odessa. Texas State Historical Association, 30. Januar 2021, abgerufen am 30. Januar 2021 (englisch). Odessa. In: Earth Impact Database. Abgerufen am 30. Januar 2021. Weblinks History of the crater. In: odessameteorcrater.com. Abgerufen am 30. Januar 2021.
Odessa Meteor Crater

The Odessa Meteor Crater is a meteorite crater in the southwestern part of Ector County, southwest of the city of Odessa of West Texas, United States. It is accessible approximately 3 mi (5 km) south of Interstate 20 at Exit 108 (Moss Road). This is one of three impact crater sites found in Texas, the others being the older and much larger Sierra Madera crater and the Marquez crater. The Handbook of Texas Online describes the Odessa meteor crater as the largest of several smaller craters in the immediate area that were formed by the impact of thousands of octahedrites (an iron metallic type) that fell in prehistoric times. The web site of the University of Texas of the Permian Basin (UTPB, Center for Energy and Economic Diversification), identifies five craters at the Odessa site and shows a distribution map of the meteorite fragments recovered from the area. The recoveries have generally come from an area to the north and northwest of the main crater site, with only a few found to the south. They indicate that the structure of the main crater, because it was one of the earliest to be recognized and studied, is now used to name similar impact sites on a worldwide basis. Over 1500 meteorites have been recovered from the surrounding area over the years, the largest of which weighed approximately 300 lb (136 kg), but excavations in the main crater confirm that there is no meteorite mass underground and probably never has been. The site has been designated as a National Natural Landmark by the National Park Service, and a small information area and nature trail has been set up on-site for a self-guided tour. It is 550 ft (168 m) in diameter and the age is estimated to be around 63,500 years (Pleistocene or younger). The crater is exposed to the surface, and was originally about 100 ft (30 m) deep. Because of subsequent infilling by soil and debris, the crater is currently 15 ft (5 m) deep at its lowest point, which provides enough relief to be visible over the surrounding plains, but does not offer the dramatic relief found at the more famous Meteor Crater in Arizona. An iron meteorite fragment was first discovered in 1921 and described in the American Journal of Science in 1922; the depression where the meteorite was found was first described as a crater in 1927. The crater itself and the museum curator, Tom Rodman, were featured in the June 1, 2013 broadcast of Bob Phillips's syndicated television series Texas Country Reporter. See also References External links Media related to Odessa Meteor Crater at Wikimedia Commons Odessa Meteor Crater and Museum website UTPB Center for Energy and Economic Diversifications, Odessa Meteor Craters Mindat.org - Odessa Craters, Odessa, Ector Co., Texas, USA Article about the crater Public domain images of West Texas and the Llano Estacado Video of the main crater site.
Cráter de Odesa

El cráter de Odesa es un cráter meteorítico situado en la parte suroeste del condado de Ector, al suroeste de la ciudad de Odesa, en el oeste de Texas (Estados Unidos). Se encuentra a unos 5 km al sur de la Interestatal 20, en la salida 108 (Moss Road).​ Se trata de uno de los tres cráteres de impacto que hay en Texas; los otros son el cráter de Sierra Madera, más antiguo y mucho más grande, y el cráter de Márquez. El Handbook of Texas Online describe el cráter meteorítico de Odesa como el mayor de varios cráteres más pequeños situados en las inmediaciones, formados por el impacto de miles de octaedritos —un tipo de meteorito de hierro metálico— que cayeron en la prehistoria.​ Se considera que el cráter de Odesa es el segundo que se ha documentado en la superficie terrestre. Esto ha dado lugar a que los cráteres con características de impacto similares —cráteres simples— también reciban el nombre de «cráteres de Odesa».​ A lo largo de los años se han recuperado más de 1 500 meteoritos —en su mayoría procedentes del norte y del noroeste— de los alrededores, el mayor de los cuales pesaba aproximadamente 136 kg. Tiene un diámetro de 168 m y se estima que su antigüedad ronda los 63 500 años (Pleistoceno o más reciente).​El cráter está expuesto en la superficie y, en un principio, tenía unos 30 m de profundidad. Debido al posterior relleno de tierra y escombros, el cráter tiene actualmente 5 m de profundidad en su punto más bajo, lo que sigue proporcionando suficiente relieve como para ser visible sobre las llanuras circundantes. En 1921 se descubrió por primera vez un fragmento de meteorito ferroso, que se describió en la revista American Journal of Science en 1922; la depresión en la que se halló el meteorito se describió por primera vez como un cráter en 1927.​​ Referencias
Cratère d'Odessa

Le cratère d'Odessa est un cratère d'impact situé dans le Comté d'Ector au Texas, au sud-ouest de la ville d'Odessa. Le diamètre du cratère principal est de 168 m et sa profondeur de 30 m; on trouve quatre petits autres cratères à proximité. Son âge est estimé à 63 500 ans. Il a été découvert en 1892 par un éleveur de bétail de la région. Sur le site se trouve un musée consacré au cratère et exposant des fragments de la météorite. Notes et références Voir aussi Liens externes « Welcome to The Odessa Meteor Crater », sur odessameteorcrater.com (consulté le 31 mai 2023) Portail du Texas Portail de la géologie
Odessa Meteor Crater

Odessa Meteor Crater è un cratere di origine meteoritica situato in Texas, Stati Uniti. Si tratta del secondo più grande cratere di origine meteoritica degli Stati Uniti. Descrizione del sito Il cratere misura 165 metri, di diametro ma nel punto centrale è profondo solo 5 metri perché nei secoli si è riempito di sabbia e detriti. Nelle vicinanze sono stati individuati altri 4 crateri, molto più piccoli, formatisi in seguito all'impatto di frammenti staccatisi dal corpo principale del bolide durante la caduta. Il meteoroide originale era composto di una solida lega di Ferro e Nichel e infatti per anni sono stati recuperati nel sito frammenti di questo meteorite. Questi esemplari sono conosciuti con il nome di meteoriti Odessa. La caduta che ha dato origine al cratere sarebbe avvenuta circa 63.500 anni fa (datazione con un errore di ± 4.500 anni). Storia Negli anni '20, dopo il ritrovamento dei primi frammenti meteoritici, fu riconosciuta l'origine meteoritica del Cratere Odessa ad opera di Daniel Barringer, l'ingegnere minerario famoso per aver riconosciuto per primo l'origine meteoritica del famoso Meteor Crater. Negli anni '30 e '40 venne fatta una sistematica esplorazione del sito con impianti di perforazione al fine di individuare eventuali masse metalliche all'interno del cratere, ma senza successo. La massa principale del meteorite originale si era vaporizzata nell'impatto, lasciando dietro di sé solo piccoli frammenti. Note Voci correlate Crateri da impatto sulla Terra Altri progetti Wikimedia Commons contiene immagini o altri file su Odessa Meteor Crater Collegamenti esterni (EN) Odessa Meteor Crater, su Enciclopedia Britannica, Encyclopædia Britannica, Inc. (EN) Odessa Meteor Crater, su Geographic Names Information System, USGS.
Odessa (krater)

Odessa – krater uderzeniowy w stanie Teksas w USA. Krater jest widoczny na powierzchni ziemi. W pobliżu miasta Odessa w Teksasie znajduje się zgrupowanie pięciu małych kraterów uderzeniowych. Główny krater ma 165 m średnicy; powstały one nie dawniej niż 63,5 tysiąca lat temu (plejstocen). Utworzył go upadek meteoroidu, który uderzył w skały osadowe. W miejscu upadku w 1922 roku znalezione zostały meteoryty żelazne z grupy I AB o łącznej masie 1,3 tony. Są to młode kratery, w niewielkim stopniu uległy wietrzeniu. Fragmenty meteorytów zostały znalezione zarówno w kraterze, jak i w wyrzuconej z niego materii, odnaleziono także tektyty, jednak ze względu na względnie małą energię uderzenia (o czym świadczy mały rozmiar) nie ma świadectw szokmetamorfizmu, które jednoznacznie dowodzą pochodzenia uderzeniowego. Miejsce uderzenia jest ogrodzone, wokół krateru i do jego wnętrza prowadzą ścieżki edukacyjne. W pobliżu głównego krateru zostało założone muzeum, prezentujące historię miejsca oraz meteoryty z tego i innych kraterów na Ziemi. Zobacz też Lista kraterów uderzeniowych w Ameryce Północnej Przypisy
Mansfield Dam

Mansfield Dam (formerly Marshall Ford Dam) is a dam located across a canyon at Marshall Ford on the Colorado River, 13 miles (21 km) northwest of Austin, Texas, United States. The groundbreaking ceremony occurred on February 19, 1937, with United States Secretary of the Interior Harold L. Ickes attending. The dam was a joint project by the Lower Colorado River Authority (LCRA) and the United States Bureau of Reclamation, with partial funding provided by the Public Works Administration. Brown and Root, headed by James E. Walters Sr., was the prime contractor. The dam was completed in 1941. Originally called Marshall Ford Dam, the name was changed in 1941 in honor of United States Representative J.J. Mansfield. The reservoir behind Mansfield Dam is named Lake Travis. The dam is owned and operated by the LCRA. Mansfield Dam is 278 feet (85 m) high, 7,089 feet (2 km) long, and 213 feet (65 m) thick at the base. The concrete gravity dam with embankment wings and saddle dikes was designed to control flooding; to store 1.4 km3 (369 billion US gallons) of water; and to generate hydroelectric power (108 megawatts). The Spillway Elevation is 714 feet (218 m) above Mean Sea Level (MSL). LCRA begins to open floods gates when water reaches 681 feet above MSL. At 681 feet (208 m) above MSL, discharge capacity exceeds 130,000 cubic feet per second (3,700 m3/s) as the lake rises. The two lanes of Mansfield Dam Road, formerly RM 620, traverse the top of the dam, but traffic other than service vehicles are now prohibited. 620 was rerouted in 1995 to a four-lane highway bridge on the downstream side of the dam built for increase in traffic due to the popularity in Austin of recreating at Lake Travis. Political History Lyndon B. Johnson ran for his first elected office as United States Representative for Texas's 10th congressional district (where the Mansfield Dam was located). His campaign was backed by the dam's contractors, and his success in clearing funding and regulatory hurdles for the dam shortly after his election is considered a cornerstone of his future political career. See also List of dams and reservoirs in Texas References External links LCRA Website Current Water Level Conditions [1]
ГЕС Менсфілд

ГЕС Маршалл-Форд — гідроелектростанція у штаті Техас (Сполучені Штати Америки). Знаходячись між ГЕС Марбл-Фоллс (32 МВт, вище по течії) та ГЕС Том Міллер (17,3 МВт), входить до складу каскаду на річці Колорадо, що впадає до Мексиканської затоки за сто двадцять кілометрів на південний захід від Х'юстона. У межах проєкту долину річки перекрили комбінованою греблею висотою 85 метрів та довжиною 2161 метр, яка включає центральну бетонну ділянку (потребувала 1406 тис. м3 матеріалу) та бічні насипні частини. Вона утримує водосховище Тревіс з площею поверхні 76,6 км2 та об'ємом 1357 млн м3 (ще 971 млн м3 зарезервовано на випадок повені). Основне обладнання станції становлять три турбіни типу Френсіс, які живляться через водоводи діаметром по 4,9 метра, мають загальну потужність 108 МВт та працюють при напорі 57 метрів. У 1943—1967 роках середньорічний виробіток станції становив 149 млн кВт·год електроенергії. Примітки
Mansfield High School (Mansfield, Texas)

Mansfield High School is a public secondary school located at 3001 East Broad Street in Mansfield, Texas, United States. Part of the Mansfield Independent School District, the school serves a portion of Mansfield. As of 2018, the school had 2,688 students. Mansfield High School is known for their baseball and golf sports programs. It is noted for its resistance to desegregation in a 1956 incident. Academics Mansfield High School is the top-performing high school in Mansfield, with a 96% graduation rate, and 83% proficiency in Reading and 85% proficiency in Mathematics. Mansfield offers 24 AP courses, ranging from Human Geography to Calculus BC. The average AP enrollment is 40% and the average pass rate is 46%. Feeder patterns The following elementary schools feed into Mansfield High School: Boren Brown Nash (partial) Reid Perry(partial) Norwood(partial) The following intermediate schools feed into Mansfield High School: Asa Low (partial) Orr (partial) Martinez(partial) The following middle schools feed into Mansfield High School: Wester (partial) Worley (partial) McKinzey(partial) Notable alumni Kennedy Brooks, 2017, Oklahoma Sooners football running back David Cook, Republican member of the Texas House of Representatives and former mayor of Mansfield Sam Hilliard, 2012, MLB outfielder for the Colorado Rockies Toby Onwumere, actor David Murray, YouTube content creator Lenzy Pipkins, 2012, American football player Hassan Ridgeway, 2012, American football player Stepfan Taylor, 2009, former NFL running back for the Arizona Cardinals Trystan Andrew Terrell, 2015, perpetrator of the 2019 University of North Carolina at Charlotte shooting Jordan Walden, 2006, former MLB pitcher Sean Williams, 2004, professional basketball player References Further reading Ladino, Robyn Duff. Desegregating Texas Schools: Eisenhower, Shivers, and the Crisis at Mansfield High (U of Texas Press, 1996) "Mansfield Crisis, 1956 overview" External links Mansfield High School Mansfield High School Tiger Band
Mansfield Legacy High School

Mansfield Legacy High School is a public secondary school located in Mansfield, Texas, United States. The school is a part of the Mansfield Independent School District and serves sections of the cities of Mansfield and Arlington as well as unincorporated sections of Tarrant County. Legacy is built on the location of the men’s club. When Mansfield was a small rural community (in the southeast of Ft. Worth), the Kowbell Rodeo was a popular stopping place for cowboys. The land on former US Highway 287, now Business 287, was the place to go for an indoor rodeo experience. History William H. (Bill) Hogg, a lifetime resident of Mansfield, opened the Kowbell Indoor Rodeo in 1959. Rodeos were held each Saturday night, year around. The Arena was built originally with an open roof and a canvas top that could be lowered for shelter during inclement weather. The Kowbell Rodeo closed, and the property was sold to MISD in 2004. Because of Mansfield's fast population growth, MISD administrators purchased the historic location to build the district's fourth high school. After clearing land and deciding on blueprints, newly hired principal, David Wright, formed a committee to create the school's name and mascot. Legacy fit perfectly. Broncos fit even better. In June 2006, committee members chose red and black as the colors. Legacy High School was turned over to MISD in June 2007 by the builder and school opened, with over 2,100 students, on August 27, 2007. Feeder patterns The following elementary schools feed into Mansfield Legacy High School: Holt (partial) Nash (partial) Neal Norwood (partial) Perry (partial) Ponder Sheppard Tarver-Rendon The following intermediate schools feed into Mansfield Legacy High School: Cross Timbers (partial) Martinez (partial) Orr (partial) Shepard (partial) The following middle schools feed into Mansfield Legacy High School: Howard (partial) Jobe (partial) McKinzey (partial) Worley (partial) Notable alumni Ryan Kirby (2008), Vocalist of Fit For A King Noah Syndergaard (2010), MLB All-Star pitcher Josh Doctson (2011), NFL wide receiver Tevin Mitchel (2011), NFL cornerback Rees Odhiambo (2011), NFL offensive lineman Tejay Antone (2012), MLB pitcher Kade Strowd (2015), baseball player in the Baltimore Orioles organization Jalen Catalon (2019), football player for the Missouri Tigers Tru Edwards (2019), NFL wide receiver for the Los Angeles Rams Harmoni Turner (2021), WNBA player References External links Mansfield Legacy High School Legacy's Student Newspaper
Marble Falls High School

Marble Falls High School (MFHS) is a public high school in Marble Falls, Texas, USA, and a part of the Marble Falls Independent School District. The school is classified as a 4A school by the UIL. For the 2024–2025 school year, the school was given a "B" by the Texas Education Agency. The school has an aerospace and engineering program for students interested in these career paths. References External links Marble Falls High School
Margaret Hunt Hill Bridge

Die Margaret Hunt Hill Bridge ist eine Straßenbrücke in Dallas im US-Bundesstaat Texas, die den Trinity River überquert. Sie wurde vom Stararchitekten Santiago Calatrava entworfen und im März 2012 dem Betrieb übergeben. Die Brücke ist Teil des Trinity River Corridor Project, das die Aufgabe hat, die dem Hochwasserschutz dienenden Überschwemmungsgebiete entlang des Flusses zu einem Naherholungsgebiet aufzuwerten. Sie dient der Verbesserung der Verbindung zwischen dem nördlich und südlich des Flusses liegenden Stadtteilen. Mit der bewussten Veränderung der Skyline der Stadt soll dem aufzuwertenden Stadtteil West Dallas eine neue Identität gegeben werden. Margaret Hunt Hill (1915–2007), eine Frau, die sich in der Denkmalpflege engagierte, war die Namensgeberin der Schrägseilbrücke. Am 120 m hohen in der Mitte stehenden Stahlbogen ist das Brückendeck mit 58 Seilen aufgehängt, die mit ihrer geschwungenen Anordnung der Brücke einen eigenständigen Charakter geben. Weblinks Einzelnachweise