One guy thrusted what looked like an aardvark at us.
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She poked the brush and thrusted the stick in holes in tree trunks.
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He thrusted the issue towards the mainstream during his 2016 primary battle against Hillary Clinton.
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It'll be Avery's first television interview since Netflix's Making a Murderer thrusted him into the spotlight.
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After a weekend of friends, family, and ideally, naps, you're thrusted into deadlines, meetings, and spreadsheets.
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We are born empty and clear and then have thrusted upon us names, ideas, preferences, et cetera.
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In 1959, a documentary called "The Hate That Hate Produced," thrusted the group into the national consciousness.
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As I thrusted I looked into his eyes, searching for any light, understanding of what was happening here.
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She said he thrusted his penis in her face, forcing her to touch it when she pushed him away.
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When she played her hit "Green Light" and everyone thrusted their phones in the air, Snapchat combined the clips.
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After she made several more attempts to escape, she claims Trump mocked her and thrusted his genitals at her.
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When Luke Cage debuted on Netflix last year it marked the beginning of a shift that thrusted Black heroes into my purview.
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In a separate incident, Weinstein allegedly "thrusted her hand onto his penis" after a movie premiere, the court documents published by Variety claim.
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It was inspiring to see this talented woman doing her thing and not being thrusted into the spotlight just because of her gender.
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Critics allege that Comey's attacks against Trump have thrusted the FBI into a partisan spotlight that could hurt the reputation of the investigative agency.
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London police have closed the case on Thursday of a jogger who thrusted a woman onto a bus lane -- after they've exhausted more than 50 leads, reports said.
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It's not often that I turn up for a press event to be told: "You're looking fabulous darling," as a glass of champagne is thrusted immediately into my hand.
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Walker thrusted herself into the lives of the major characters on the show, picking up a few relationships along the way and one longstanding feud Alison Sweeney's character Sami Brady.
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Whether Sanders starts raising the issue regularly on the campaign trail could help determine whether it stays on the fringe or if its thrusted towards the center of political debate.
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" The report states that Tony T reached out from behind the camera and choked her; at another point, Nomar thrusted into her so violently her "blood splattered on the white walls.
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It is hard to dispute that a long bladed weapon that can be swung or thrusted wildly from half a metre away isn't handy to have in a life or death altercation.
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At one point, a svelte dancer stripped off his leather thong and thrusted his hips to Benny Benassi's "Satisfaction" while erecting a crucifix against his groin, his dick perfectly tucked between his legs.
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The Washington Post said Wednesday, citing officials and outside advisors, his team had been thrusted into "chaos" after revelations of a meeting between Donald Trump Jr. and a lawyer characterized as linked to the Russian government.
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READ MORE: Cleanse Your Aura with the Power of Eggs This whole affair reminds us an awful lot of that classic Aboriginal folklore in which Brolga the dancing bird thrusted Dinewan the Emu's egg into the sky and thus created the sun.
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The death of Associate Justice Antonin Scalia, the conservative beacon on the high court who served for three decades after being confirmed unanimously by the Senate in 1986 as a Reagan appointee, has thrusted the third branch of government into the national spotlight.
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A New York Times report Saturday unveiled that a Yale classmate of Kavanaugh's, Max Stier, told the FBI and Senators that he'd once seen Kavanaugh take his pants down at a party and that his friends thrusted his penis into a woman's hand.
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The big picture: The Times reported Saturday that a Yale classmate of Kavanaugh's, Max Stier, told the FBI and Senators that he had seen Kavanaugh take his pants down at a party and that his friends thrusted his penis into a woman's hand.
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Ovechkin has won the Rocket Richard Trophy as the NHL's top goal scorer six times in his career (including the last four seasons), so it's only fitting that his 1,213th point and 545th goal thrusted him ahead of Maurice Rocket Richard on the all-time goals list.
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Read more: The 4 Democratic presidential candidates who cosponsored Bernie Sanders' Medicare for All Senate bill either no longer support it or won't say if they doSanders has long advocated for Medicare for All, a signature issue he thrusted towards the political mainstream during his insurgent primary run in 2016.
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"For 10 years I have been the best father I could be, all while quietly being on the receiving end of constant toxic false accusations by the mother of my child and of course all the while being thrusted into unexpected social media storms all while trying to fight for my career and stay afloat financially," he said.
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Inexplicably, a teal-tulle-tangled The Vixen, who looked and thrusted about like a suburban teenager at an '80s themed frat party, was named winner of the challenge (in a tie with the more deserving Asia O'Hara, who eased on down the hay-strewn road looking like the love child that Diana Ross and Michael Jackson never had).
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39 To the west of Paz de Río, the Cuche Formation is thrusted upon the Neogene Concentración Formation by the Soapaga Fault.
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All of these lithologies were folded and thrusted, so that the basement rock can be found on top of the sediments and vice versa.
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The Columbus basin is bounded by the Darien Ridge, part of the uplift region in the north west, which separates the thrusted area from the extended section to the southeast.
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The Helvetic nappes are thrusted over the Infrahelvetic complex and the external massifs of the Alps (like the Aarmassif or Mont Blanc Massif). In Switzerland, Germany and Austria they are also thrusted over the Molasse basin of the Alpine foreland. In turn, the Helvetic nappes were overthrusted by the Penninic nappes from the south. In Switzerland these have been eroded away at most places but in Germany and Austria they are still covering the Helvetic nappes.
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The Rybachy Peninsula in northern Murmansk Oblast hosts Jotnian sedimentary rocks dated to have sedimented 1126±50 million years ago. These rocks are thrusted over by younger Vendian and Upper Riphean rocks.
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Meanwhile, at the surface the upper crust of the Adriatic plate (the later Austroalpine nappes) was thrusted over the European crust. This was the main collisional phase in the formation of the Alps.
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24 (4): 277-289. After allegations of female infidelity or separation from their partner, both men and women report that men thrusted the penis more deeply and more quickly into the vagina at the couple's next copulation.
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The Austroalpine nappes are a geological nappe stack in the European Alps. The Alps contain three such stacks, of which the Austroalpine nappes are structurally on top of the other two (meaning they were thrusted over the other two). The name Austroalpine means Southern Alpine, because these nappes crop out mainly in the Eastern Alps (the Alps east of the line Lake Constance - Chur – Lake Como). Because the Austroalpine nappes consist of material from the former Apulian or Adriatic plate, that was thrusted over the European plate, they are called allochthon nappes.
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The rocks were formed at a passive margin of the Paleo-Tethys Ocean, when the Austroalpine terrain was part of the micro-continent Avalonia. Together with the other Austroalpine units, they were thrusted over the European plate during the Alpine orogeny.
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Thrust and reverse fault movement are an important component of mountain formation. fold that thrusted. Mountain formation refers to the geological processes that underlie the formation of mountains. These processes are associated with large-scale movements of the Earth's crust (tectonic plates).
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Wiesner Ceballos et al., 2007, p.16 The Guadalupe Group is thrusted on top of the younger Guaduas, Bogotá and Cacho Formations by the Bogotá Fault.Geological Map Bogotá, 1997 The NNW-SSE trending eastward dipping thrust fault forms a barrier for aquifers.
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Meanwhile, the thrust front of the Penninic and Austroalpine nappes moved on, pushing all material in its way northward. Due to this pressure a decollement developed over which thrusting took place. The thrusted material would become the Helvetic nappes. Adriatic plate started rotating counterclockwise.
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The Outer Western Carpathians were formed during orogeny that took part since the Upper Cretaceous (Senonian) and Miocene periods, which is later than the Central Western Carpathians. Pieniny Klippen Belt was affected by thrusting together with the Central Carpathians and later folded and thrusted again together with the Flysch Belt.
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Flysch units from the Cretaceous to Early Miocene are located between the External and Internal Zones. These were folded and thrusted during the westward migration of the Internal Zones and can be interpreted as the palaeo-accretionary wedge of the subduction system that was active during the Lower and Middle Miocene.
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Chuojiao (thrusted-in feet) In chapter 29 of Water Margin, titled "Wu Song beats Jiang the Door God in a drunken stupor", it mentions Wu Song, another of Zhou's fictional students, using the "Jade Circle-Steps with Duck and Drake feet".Shi, Nai’an and Luo Guanzhong. Outlaws of the Marsh. Trans. Sidney Shapiro.
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The Helvetic zone consists of a number of tectonically very different units. The "Helvetic nappes" are a nappe stack that was thrusted over the molasse of the Molasse basin in the Alpine foreland. They are composed of Mesozoic marine limestone, marls and shales. The Helvetic nappes are completely detached from their former basement.
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Most exposed rocks in the suture zone are thrusted accretionary wedges, often with ophiolites. Uranium-lead dating of basalt, dolerite gabbro as well as Silurian radiolarite gives ages constraints on the formation of the oceanic crust. Dated rocks in the Adaatsag ophiolite in the east are among the oldest at 325 million years old.
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The Abitibi greenstone belt is one of the world's largest Archean greenstone belts. It represents a series of thrusted subterranes that exhibit similar geological, geochemical, and isotopical signatures similar to those formed during the evolution of paired active-arc-back-arc systems. The huge 2,707-to-2,696-million-year-old Blake River Megacaldera Complex is within the belt.
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The Subvariscan Zone north of the Rhenohercynian Zone was untouched by Hercynian metamorphism. During the Hercynian orogeny, the Rhenohercynian zone was folded and thrusted internally. It was thrust over the foreland to the north (the London-Brabant Massif and other Avalonian terranes). From the south it was overthrust by the Mid-German Crystalline High, part of the Saxothuringian Zone.
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Occasionally, the large blocks of crust are rotated and thrusted along deep-rooted thrust faults. This process may expose a cross-section of crust to the surface, as at Euboea Montes. Later, these blocks can also be eroded by mass wasting and reburied by subsequent volcanism. At the base of the crust, materials are met again by heat.
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In addition to short swords, Roman infantry typically carried a spear or other type of pole weapon. The most common was known as the javelin, a heavy spear that could be either thrown or thrusted. Similar in function to the javelin was the fuscina. Although not used by the Roman military, this fork-like trident was one of the most popular gladiator weapons.
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These rocks are often thrusted over the alluvial rocks of the sub-Himalaya. The Lesser Himalaya also contains granites and felsic volcanic rocks. The Central Himalayan Domain contains rocks from the Tethys Ocean and is also intruded by Miocene granites, related to the formation of the Himalaya. The Indus Suture Zone is the suture zone with the Lhasa terrane to the North.
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The Helvetic nappes () are a series of nappes in the Northern part of the Alps and part of the Helvetic zone. They consist of Mesozoic limestones, shales and marls that were originally deposited on the southern continental margin of the European continent. During the Alpine orogeny they were thrusted north over a décollement and at the same time were internally deformed by folding and thrusting.
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Covering a surface of in the south-eastern region of the Po Valley, the Ponte dei Grilli exploration permit was awarded March 2009. Also on trend with large existing fields, the exploration targets in the Ponte dei Grilli permit area are gas accumulations trapped in thrusted anticlines, stratigraphic pinch outs and structural features in the Plio-Pleistocene turbiditic sands located in the Apennines foredeep.
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The zone consists of the Tatra-Fatra Belt of core mountains, the Vepor Belt, and the Gemer Belt. In their predominantly crystalline basement zones called the Tatric, Veporic, and Gemeric, thrusting (thick-skinned) is also present, but not as apparent. Geophysical investigation confirmed that the Gemeric is thrusted over the Veporic, and the Veporic over the Tatric.Tomek, Č., 1993: Deep crustal structure beneath the central and inner West Carpathians.
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The Gemer Belt is a zone of predominantly crystalline rock, partially thrusted over the Veporic. The most important portion of the zone is the Gemeric unit, unlike the other Carpathian units with signs of low grade (greenschist facies) Hercynian metamorphic overprint. The Gemeric is the uppermost basement- involved unit of the Central Western Carpathians. It is made by phyllites, quartzites, porphyrys and limestones commonly metamorphosed to siderite and magnesite.
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To the east the Yerrida and Earaheedy Basins were passive margins along the Yilgarn's northern margin. The c. 1830 Ma phase of the Capricorn Orogeny resulted in northeast- southwest deformation of the Bryah-Padbury Basin with flood basalts in the Yerrida Basin. The Gascoyne Complex rocks, namely the Yarlarweelor Gneiss are thrusted eastward onto the upper rock units of the Bryah Basin and the whole succession of the Padbury Basin.
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The oldest rocks are in the Scotland Formation and include Eocene age turbidite and radiolarites. This unit is 4.5 kilometers thick from the sea floor to the surface. It is overlain by a syncline basin called the Woodbourne Trough, which includes pelagic sediments. Nappe formations of the Oceanic Formation, from a Miocene forearc basin filled with calcareous pelagic sediments and volcanic ash is thrusted on top of the two older units.
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Caledonian rocks overlie rocks of the much older Svecokarelian and Sveconorwegian provinces. The Caledonian rocks actually form large nappes () that have been thrusted over the older rocks. Much of the Caledonian rocks have been eroded since they were put in place meaning that they were once thicker and more contiguous. It is also implyed from the erosion that the nappes of Caledonian rock reached once further east than they do today.
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It is the spot behind/below the ear lobe. Once the blade is stabbed to about two inches, it must be thrusted and twisted upward in ninety degrees. If correctly performed, the victim might try to scream and gasp for air but it will not be possible. The only sound will be the victim's physical struggle, which was already taken care of if the assailant attacked from behind.
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The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch. With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago. Frosty Mountain is composed of vertically thrusted metasedimentary rock from the ancient Methow Ocean.
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The Moldanubian Zone was introduced by German geologist Franz Kossmat in 1927. It has a generally higher grade of metamorphism than the Saxothuringian Zone to the northwest. The contact between the two is a thrust over which the Moldanubian Zone moved over the Saxothuringian Zone during the Variscan Orogeny. In the east the Moldanubian Zone is thrusted over the Moravo-Silesian Zone, which is also generally lower grade.
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The Helvetic nappes are thrusted over the "Infrahelvetic complex" in eastern Switzerland. The Infrahelvetic complex is composed of autochthonous Mesozoic sediments on top of Hercynian basement rock. The Mesozoic of this unit is contemporary with that of the Helvetic nappes, but deposited further north on the former continental slope and therefore shallower in sedimentary facies. The Infrahelvetic is internally deformed by thrusting and folding that continues into the Hercynian basement.
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The onset of Andean orogeny first caused the basin to rise and dry up with red beds being deposited in its eastern part. Then the sedimentary basin was subject of a complete basin inversion. During deformation Chonta Fault acted as a barrier "damming-up" folded and thrusted strata west of it. This makes the fault define the limits of two different styles of thin-skinned deformation within the belt.
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Vršatec klippe, in Slovakia is the largest Czorsztyn type klippe The Pieniny Klippen Belt is divided into numerous tectonic units, but only few of them occur throughout the entire belt. The oldest rocks of the Klippen belt are Middle Jurassic to upper Cretaceous. They are in normal stratigraphical positions, with only minor hiatus. Large scale crustal shortening caused rocks of different tectonic units and origin to be thrusted over each other and now lying juxtaposed.
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The two men battled back and forth for ten days, but neither could take the upper hand. After Fu Jian reached Tongbi (銅壁, in modern day Tongchuan, Shaanxi), Zhang Ping went all out with his army. Zhang Ci successfully charged into enemy lines for more than four times, breaking their formation. It was not until Fu Jian's general Lü Guang, who thrusted his spear into Zhang Ci, that he could be stop.
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The main fault in the Eastern Hills is the longitudinal eastward dipping thrust fault called the Bogotá Fault, striking north-northwest to south-southeast, parallel to the longitudinal axis of the Eastern Hills. It forms the tectonic limit with the Bogotá savanna and acts as a barrier for aquifers.Velandia & De Bermoudes, 2002, p.42 The compressional tectonics thrusted the Cretaceous units of Guadalupe and Chipaque on top of the younger Guaduas, Cacho and Bogotá Formations.
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The Cape Supergroup rocks were deposited in a purely marine setting, within a wide passive margin basin known as the Cape Basin. The rocks were deposited over a 170-million-year period ranging from approximately 485 Ma (Tremadocian) to the Early Carboniferous (about 330 Ma; late Mississippian). Up to of strata were preserved throughout. The Cape Supergroup rocks later underwent deformation during the Cape orogeny, in which the rocks were folded and thrusted upwards.
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During the collision with the Superior province, the MRV gneissic block was thrust up onto the Superior province's edge; this resulted in a thrusted crumpled fault tens of kilometers wide producing a mountain range, and a shear zone which defines the boundary between the two terranes. Tectonism along the zone began during the docking of the two terranes into a single continental mass, and culminated in the early Proterozoic, where deformation took place under low to intermediate pressures.
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About 75,000 years ago glaciers moved down the sides of what became Pikes Peak. Over time, the ground also thrusted upward. The combination of the change in terrain from the moving tectonic plates and the sculpting of rock due to the moving boulders created the steep canyons of the Ute Pass entrance. From the entrance of Ute Pass at Manitou Springs and for about 5 miles, the terrain is steep canyon land and the road has many curves.
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Inversion of the basin took place in the Upper Cretaceous and was accompanied by intrusion of a small body of granite. In addition to nappe outliers of the Choč nappe (Hronic) and part of the Krížna nappe (Fatric), there is also a large body of Muráň nappe (Silicic unit). The Veporic is partially thrusted over the Tatric and lies under the Gemeric unit. The nappe stack of the Veporic and Gemeric later collapsed and evolved in the Veporic metamorphic core complex.
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Guadalupe Hill is the type locality of the Guadalupe Group, a Late Cretaceous sedimentary sequence of sandstones and shales of thick. The formation is thrusted on top of younger strata by the reverse Bogotá Fault during the Andean orogeny. The hill is the source for the Manzanares and El Chuscal creeks that flow westwards onto the Bogotá savanna. Historically, Guadalupe Hill was an important sacred site for the indigenous Muisca, who inhabited the Bogotá savanna and surrounding regions before the Spanish conquest.
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Paleogeographic reconstruction of the supercontinent Pangaea, including the Central Pangean Mountains of which the Mauritanide Belt formed part of. The Mauritanide Belt is an ancient orogen running parallel to the west coast of Africa from Morocco to Guinea-Bissau. The orogeny that formed the Mauritanide Belt was active between 320 and 270 million years ago in the Carboniferous and Permian. During this time period the eastern nappes of the belt thrusted over rocks of Devonian age in the Taoudeni Basin.
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During the Late Cretaceous and early Cenozoic, the Indian plate drifted northward a vast distance resulting in the closure of the Neo-Tethys Ocean. Approximately 40-50 million years ago remnants of the ocean vanished as India collided with the Eurasian plate. As the continental plates are relatively low density they cannot be subducted. This results in the Eurasian plate being thrusted up leading to the rise of the Tibetan Plateau, bounded to the south by the collisional Himalayan mountain range.
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According to Garciacaro et al., the foreland basin was created by flexural subsidence at the passive margin of the colliding regions of the Caribbean and South American plates. The collision created loading of thrusts and folds which led to subsidence in the basin and contributed to the complex faulted and thrusted nature of the foreland basin formed. The Orinoco River delta has been the major source of siliciclastic sediments for the basin, with deposition within the basin beginning in the early Miocene.
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If using low-thrust engines such as electrical propulsion to get from the transfer orbit to geostationary orbit, the transfer orbit can be supersynchronous (having an apogee above the final geosynchronous orbit). However, this method takes much longer to achieve due to the low thrust injected into the orbit. The typical launch vehicle injects the satellite to a supersynchronous orbit having the apogee above 42,164 km. The satellite's low- thrust engines are thrusted continuously around the geostationary transfer orbits in an inertial direction.
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In the period after the Eocene the Northern Peruvian Andes were subject to the Quechua Phase of orogeny. The Quechua Phase is divided into the sub-phases Quechua 1, Quechua 2 and Quechua 3. The Quechua 1 Phase lasted from 17 to 15 million years ago and included a reactivation of Inca Phase structures in the Cordillera Occidental. 9–8 million years ago, in the Quechua 2 Phase, the older parts of the Andes in northern Peru were thrusted to the northeast.
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In the Paleocene and the Eocene, the North Mesotethys Ocean closed, forming the Shachrud-Nishapoor thrusted-folded arc and the Eastern Iran transverse folded system. This led to the incorporation of Turkmenistan, Iran and Afghanistan into the larger Eurasian Plate. As Gondwana moved northward and interacted with Eurasia in the Paleogene, subduction began south of the current Zagros Mountains in northern Iraq and Iran. As the North Mesotethys Ocean basin was subducted, it kicked off calc-alkaline volcanism in Iran in the Eocene.
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Tectonic map of the Mediterranean, showing the position of the Alps within other structures of the Alpide belt The Alps form a northward convex arc around their southeastern foreland basin, the Po river basin (to be precise the south is in fact their hinterland). Quaternary and Neogene sediments in this basin lie discordant over the southernmost thrust units. In the northeast, southward dipping and internally thrusted Cenozoic foreland deposits (flysch and molasse) are found. This Bavarian and Swiss foreland basin is called the Molasse basin.
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The 2003 Boumerdès earthquake The geology of Algeria is diverse; the country divides into three different tectono-stratigraphic domains. In the south and west is the West African Craton which consists of Precambrian granitic basement and surrounding Neoproterozoic mobile belts. Further south the Tuareg Shield comprises the Hoggar, Adrar des Iforas and Air sub-shields which have each been affected by tectono-thermal events touching much of the continent. In the north are the Alpine chain mountains with a succession of folded and over-thrusted strata.
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Sites, Op. cit. Overall, this region reveals the interior of this thrusted anticlinal- synclinal structure and presents a phenomenal exposure of complex central Appalachian macroscale structures involving the Silurian-Devonian package of rocks. Geologically, the Smoke Holes are the most uniquely exposed region within the westernmost central Appalachians and they have served as a surface model for complex subsurface structures shown and/or suspected by seismic and exploratory drilling. Furthermore, this region provides detailed insight into the lowermost roof-sequence cover above the suspected duplex of Cambrian- Ordovician horse-blocks and blind-thrusts at depth.
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Of India funded by the World Bank. In 2007, the institute received a final feather to its cap when the Union Government of India declared it as an “Institute of National Importance”. The institute receives significant funding every year from the Government of India which is usually spent for research, improving the infrastructural facilities in the campus and to bring international standards. On 22 November 2013, during the institute's 9th convocation, Shri Pranab Mukherjee, President of India addressed the Institution and appreciated its efforts in thrusted Research and innovation.
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The stratigraphy of the Widgiemooltha Komatiite is well known to be part of the regional komatiite magmatic event also seen at the Kambalda Dome, to the north. There are comparisons which place the Widgiemooltha Komatiite as equivalent to the Silver Lake Komatiite. The Mt Edwards Basalt is correlated regionally with the Devon Consuls Basalt of Kambalda, and the Widgeimooltha Chert correlated with the Paringa Slate. The structure of the Widgiemooltha Dome has three thrusted repetitions of the basal komatiite contact and komatiite sequence including footwall Mt Edwards Basalt and hangingwall sediments (Widgiemooltha Chert).
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Geologic map of the southeastern part of the Rhenish Massif, showing outcrops of the Giessen nappe in orange. The Giessen nappe has the same colour as the Hörre zone, which is on the other, northwestern side of the Lahn syncline. The Giessen nappe () is a tectonic nappe in the southeastern part of the Rhenish Massif in western Germany. The nappe is an "alien" (allochthonous) unit in the Rhenohercynian zone of the Hercynian orogeny, it was thrusted over the usual slightly metamorphosed Devonian and Carboniferous sedimentary rocks in this zone.
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Martinsloch The Glarus thrust () is a major thrust fault in the Alps of eastern Switzerland. Along the thrust the Helvetic nappes were thrusted more than 100 km to the north over the external Aarmassif and Infrahelvetic complex. The thrust forms the contact between older (Helvetic) Permo-Triassic rock layers of the Verrucano group and younger (external) Jurassic and Cretaceous limestones and Paleogene flysch and molasse. The Glarus thrust crops out over a relatively large area in the cantons Glarus, St. Gallen and Graubünden, due to its horizontal orientation and the high local relief.
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Its universal application was thrusted through the use of traditional growth rods which required repeated invasive surgeries every 6-12 months for the sustenance of growth, via distraction. Nowadays developed countries only use MAGEC (MAGnetic Expansion Control) rods to non-invasively lengthen the spine. In contrast, developing and under-developed countries still use traditional growing rods, which require invasive surgery every 6-12 months, because of high initial cost associated with procurement of MAGEC rods. Compression-based system include tethering using a flexible rope-like implant and are relatively new to receive FDA approval.
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The obduction of ophiolites is interpreted as the closure of several Neo- Tethys between the Shan-Thai block, Burma microplate and Indian Plate. The sedimentary sequence overlain by the ophiolites ranges from Late Triassic to Orbitoides-bearing Late Cretaceous carbonates and shales, where part of the sedimentary sequence has undergone high pressure/low temperature blue-schist metamorphism. The pre-Triassic metamorphic basement composed of Kampetlet schist and gneisses were exposed in the Mount Victoria area in Myanmar. The flysch type sediments in the western flank of the Indo-Burman Range are relatively younger than the folded and thrusted eastern flank.
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During a collisional orogeny, these Paleozoic and Mesozoic rocks were uplifted, thrusted and folded as the Central Guatemalan Cordillera. Paleogene rocks from the early Cenozoic include volcanic and marine clastic rocks, associated with high rates of erosion. By contrast, to the south of the Motagua Valley, the underlying rocks belong to the Chortis Block—the northern section of the Caribbean Plate. Many geologists have interpreted the Chortis Block as having "translated" eastward to its present position, with Cretaceous brittle deformation and uplift suggesting a connection to the Laramide orogeny building up the Rocky Mountains to the north.
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Floridablanca is situated at an altitude of about in the Eastern Ranges of the Colombian Andes, though locally the topography varies greatly. To the east of the city the higher mountains of the Andes rise above the city, thrusted upwards by the north–south-trending Bucaramanga-Santa Marta Fault, one of the major megaregional faults of Colombia. The area is dominated by the Bucaramanga Nest, the second-most seismically active region in the world.Santander, el segundo nido sísmico más activo del mundo Because of the relatively low altitude, the city enjoys a very favorable climate all year round.
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8 ff. . in structural geology describes a fold belt of west and central Europe, formed during the Hercynian orogeny (about ). The zone consists of folded and thrusted Devonian and early Carboniferous sedimentary rocks that were deposited in a back-arc basin along the southern margin of the then existing paleocontinent Laurussia. The Rhenohercynian Zone, named for the Rhine River and the Hercynian Forest of Antiquity, forms a narrow zone through western and central Europe, from Cornwall and Ireland in the west to the Harz mountains of central Germany in the east, including the Rhenish Massif (Ardennes, Taunus, Eifel and Hunsrück).
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Bertrand was familiar with the Faille du Midi (Variscan orogeny), a large thrust fault in the Belgian Ardennes. Meanwhile, British geologists began to recognize the nature of thrust faults in the Scottish Highlands. In 1883, Archibald Geikie accepted that the Highlands are a thrust system. Swiss geologists Hans Schardt and Maurice Lugeon then discovered in 1893 that in western Switzerland, Jurassic rock layers are on top of younger molasse too, and argued that the structure of the Alps is a large stack of nappes, large sheets of rock that had been thrusted on top of each other.
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The full-width, forward-thrusted "eggcrate" grille was flanked by dual stacked headlights for the third consecutive year. The squarer cornered grille insert had blades that seemed to emphasize its vertical members and it appeared both above the bumper and through a horizontal slot cut into it. Rectangular parking lamps were built into the outer edges of the grille. Rear end styling revisions were highlighted by metal divided tail lamps and a painted lower bumper section. Coupe de Villes got a new roofline, inspired by the Florentine show car created for the 1964 New York World's Fair, that gave rear seat passengers added privacy.
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Thrust of the Carpathians on their foreland caused a flexure of the lower continental plate under the frontal part of the nappes. This flexured area, called the Carpathian Foredeep, was filled by thick formations of molasse, prevailingly marls, sandstones and conglomerates that were formed in the Oligocene to Miocene periods by erosion of the growing Carpathians. Nevertheless, the foredeep is not generally folded; flysch nappes thrusted from the south partially folded the rock underneath. The whole zone of the foredeep is developed in the foreland of the Alps, and runs through the Moravia to the Ostrava Basin and further East to Poland, Ukraine, and Romania.
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South of this line are folded and thrusted units of the Southern Alps. North of the Periadriatic seam, rocks from three main palaeogeographic "domains" are found: the Helvetic or Dauphinois, the Penninic and the Austroalpine domains. This subdivision is made according to the paleogeographical origins of the rocks: the Helvetic Zone contains material from the European plate, the Austroalpine Zone material from the Adriatic plate, the Penninic Zone material from the domains that existed in between the two plates.See for a detailed subdivision of the geologic units in the Alps for example , , Simplified geological map of the Alps, showing the tectonic subdivision and the largest geological structures.
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To reach the lowlands north of La Paz the Yungas-vegetated Cordillera Oriental has to be passed. The Sub-Andean Zone and the Northern and Eastern Lowlands share a common ancient history but has since the Andean orogeny developed to two distinct zones. While both zones share essentially the same old sedimentary platform strata the strata at the Sub-Andean Zone have been folded and thrusted into a fold and thrust belt with structural traps where hydrocarbon fluids have accumulated. The limit between the fold and thrust belt and the Eastern Lowlands is drawn by the Serranía del Aguaragüe a north-south range representing the Andean thrust front.
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The type section of the Paja Formation is found at the banks of Quebrada La Paja in Betulia, Santander, where the formation has a thickness of .Patarroyo & Moreno, 1997, p.30 Outcrops of the formation extend from Simití in the north, close to the border of Santander and Bolívar, where the formation is offset by the Simití Fault,Plancha 85, 2006 to the Pauna Anticlinal in San Pablo de Borbur, where the formation is thrusted over the Ritoque Formation in the south.Plancha 190, 1998 In the southern extension of the exposures, the formation crops out in the north of Tununguá, near the Ibacapí Fault.
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The improved aircraft includes a reinforced airframe, air- thrusted engines, radar, and improved avionics, while excluding canards and an air brake. The Russian Air Force designated them as the Su-35S and ordered 98 units with additional orders from China and Indonesia. Sukhoi thought sales of the Su-35S would go over 160 but they are blunted by updated versions of the Sukhoi Su-30.The leftIn May 2008, the UAC presented its third aircraft and the first airliner designed and exported under the UAC brand, the Sukhoi Superjet 100 (SSJ 100). The SSJ 100 is the fourth civilian aircraft and the first airliner to be made by Sukhoi.
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Skidoo townsite in 1906 The plutons in the park are Jurassic and Cretaceous aged and are located toward the park's western margin where they can be seen from unimproved roads. One of these relatively small granitic plutons was emplaced 67–87 Ma and spawned one of the more profitable precious metal deposits in the Death Valley area, giving rise to the town and mines of Skidoo. In the Death Valley area these solidified blobs of magma are located under much of the Owlshead Mountains and are found in the western end of the Panamint Mountains. Thrusted areas can be seen at Schwaub Peak in the southern part of the Funeral Mountains.
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This program is used to collect and analyze the high-quality data on climate change. The hope is that research based on this data is thrusted to impact near and long term policy and decision plans made by senior government and business leaders. It is being implemented and managed by the National Climatic Data Center (NCDC) located in Asheville, NC. Scientists and engineers from the Atmospheric Turbulence and Diffusion Division located in Oak Ridge, TN, are assisting the NCDC USCRN program staff. System design, test, implementation, and associated expenses are being provided by the National Environmental Satellite, Data, and Information Service's Office of Systems Development.
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Geological makeup of the Alps: The Central Alps are formed from the crystalline East Alpine and several windows, regional nappes and islands The Central Alps consist mainly of the gneiss and slate rocks of the various Austroalpine nappes (Lower and Upper Austroalpine), with the exception of the Hohe Tauern and Engadine windows, where they are composed mostly of Jurassic rock and limestones and, locally, (Bergell and Rieserferner) also of granite. The Austroalpine nappes are thrusted over the Penninic nappe stack. Massifs of autochthonous, crystalline rock, which hardly moved at all during Alpine folding, do not occur in the Central Alps – unlike the case in the Western Alps. The aforementioned granite intruded near the fracture zone of the Periadriatic Seam.
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In the mid-late Triassic, the Shan-Thai block collided with the Indo-China block, and under-thrusted an ophiolite and associated arc system in the northeast. A foreland thrust belt developed along the collision of the two blocks and laid the foundation of the Shan Plateau. A thick flysch unit with fossils and deltaic sediments were deposited along the northeastern Shan-Thai block (now Shan Plateau) with the closing of a shallow sea region between the two blocks prior to collision. Large-scale intrusion of granitoid plutons and batholiths were induced by oceanic subduction; and partial melting of metasedimentary rocks within the foreland thrust belt led to tin-tungsten mineralization (the Central Tin Belt).
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Zipa Tisquesusa – Banco de la República When Tisquesusa retreated in his fort in Cajicá he allegedly told his men he would not be able to combat against the strong Spanish army in possession of weapons that produced "thunder and lightning". He chose to return to Bacatá and ordered the capital to be evacuated, resulting in an abandoned site when the Spanish arrived. In search for the Muisca ruler the conquistadores went north to find Tisquesusa in the surroundings of Facatativá where they attacked him at night. Tisquesusa was thrusted by the sword of one of de Quesada's soldiers but without knowing he was the zipa he let him go, after taking the expensive mantle of the ruler.
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The range is northwest-by- southeast trending and is in a region of about thirty landforms, plains, valleys, and mountain ranges, called the Maria fold and thrust belt. The region is in the Basin and Range and three mountain ranges are in a parallel, northwest-by-southeast trending thrust belt, with two intervening valleys. The Granite Wash Mountains are attached to the southwest end of the Harcuvar Mountains, the center range of the 3 basin and range-thrusted mountains. The Granite Wash range is on the same water divide as the Little Harquahala's and at the southwest end of the McMullen Valley; to the east, the range and water divide forces the upland drainage areas of the Centennial Wash to turn from southwest- to southeast-flowing towards the Gila River at the Gila Bend Mountains.
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The center of the range is occupied by the Tobacco Root Batholith, thought to be a satellite pluton of the Boulder Batholith.Reid, R.R., 1957, Bedrock geology of the north end of the Tobacco Root Mountains, Madison County, Montana: Montana Bureau of Mines and Geology Memoir 36 This Late Cretaceous granitic body intrudes Archean gneisses and schists.Precambrian Geology of the Tobacco Root Mountains, Montana, John B. Brady, H. Robert Burger, John T. Cheney, and Tekla A. Harms, editors, Geological Society of America Special Paper 377, 2004 Significant gold deposits appear to be related to the intrusion of the Tobacco Root Batholith and northwest-trending faults in the Pony area and elsewhere. The northern flank of the Tobacco Roots consists of thrusted and folded sedimentary and volcaniclastic rocks ranging from Proterozoic Belt Supergroup strata to Cretaceous Elkhorn Mountains Volcanics.
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The Kula Plate began subducting under the Pacific Northwest region of North America during the Late Cretaceous period much like the Pacific Plate does, supporting a large volcanic arc system from northern Washington to southwestern Yukon called the Coast Range Arc. There was a triple junction of three ridges between the Kula Plate to the north, the Pacific Plate to the west and the Farallon Plate to the east. The Kula Plate was subducted under the North American Plate at a relatively steep angle, so that the Canadian Rockies are primarily composed of thrusted sedimentary sheets with relatively little contribution of continental uplift, while the American Rockies are characterized by significant continental uplift in response to the shallow subduction of the Farallon Plate. About 55 million years ago, the Kula Plate began an even more northerly motion.
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Gaga performing "Sexxx Dreams" during her residency, Lady Gaga Live at Roseland Ballroom (2014) "Sexxx Dreams" was one of several Artpop tracks included in Gaga's 2013 concert at the iTunes Festival in London. Ashley Percival of The Huffington Post wrote of her performance: "'Sex Dreams' made 2009's 'LoveGame' with its disco stick look like a nursery rhyme, as she delivered its racy and oh-so- Gaga lyrics." Reviewing Gaga's live performance, Gil Kaufman of MTV described the song as "theatrical, throbbing pop", with Gaga channeling "Prince, Madonna and anyone else who writhed on, humped or thrusted into a stage in the 1980s while sharing their most intimate, detailed nighttime desires." In November 2013, Gaga performed "Sexxx Dreams" at ArtRave, a two-day promotional event for Artpop, held at the Brooklyn Navy Yard in New York.
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The Torca River at the border with Chía in the north, the boquerón (wide opening) Chipaque to the south and the valley of the Teusacá River to the east are the hydrographic limits of the Eastern Hills. Geologically, the Eastern Hills are the result of the westward compression along the Bogotá Fault, that thrusted the lower Upper Cretaceous rocks of the Chipaque Formation and Guadalupe Group onto the latest Cretaceous to Eocene sequence of the Guaduas, Bogotá, Cacho and Regadera Formations. The fold and thrust belt of the Eastern Hills was produced by the Andean orogeny with the main phase of tectonic compression and uplift taking place in the Pliocene. During the Pleistocene, the Eastern Hills were covered by glaciers feeding a large paleolake (Lake Humboldt) that existed on the Bogotá savanna and is represented today by the many wetlands of Bogotá.
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The non-stiffened Francis Rogallo parawing, the Domina Jalbert founded parafoil wing, or other modified fully flexible wings (Barish sailwing, KiteShip wing, parasails, modified conical parachutes) do not lend themselves to a mounting of a prime moving engine or motor to them; rather the kiting lines to the unpowered wing terminate below the wing to a static or mobile anchoring; that anchoring itself may be with its own active thrusting engine or motor or the anchor (which could be payload, pilot, or both payload and pilot) may simply fall by gravity force—and thus by gravity tug the wing through the kite lines. When the payload or pilot is simply falling without adding a prime moving engine or motor, then the kited flexible wing is a paragliding wing; when the payload or pilotComparing Ultralight Aircraft: Choices, Choices. Author sees what is nearly a cliché by those understanding: paraglider is a kite. is additionally arranged with a thrust engine or motor, then the kited unpowered flexible wing with such thrusted payload or pilot is a powered aircraft system or powered paragliding system.
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Castile engaged later in this economic activity, rather by adhering to the incipient atlantic slave trade involving sub-saharan people thrusted by Portugal (Lisbon being the largest slave centre in Western Europe) since the mid 15th century, with Seville becoming another key hub for the slave trade. Following the advance in the conquest of the Nasrid kingdom of Granada, the seizure of Málaga entailed the addition of another notable slave centre for the Crown of Castile. By the end of the 15th century (1490) the Iberian kingdoms (including here the Balearic Islands) had an estimated population of 6.525 million (Crown of Castile, 4.3 million; Portugal, 1.0 million; Principality of Catalonia, 0.3 million; Kingdom of Valencia, 0.255 million; Kingdom of Granada, 0.25 million; Kingdom of Aragon, 0.25 million; Kingdom of Navarre, 0.12 million and the Kingdom of Mallorca, 0.05 million). For three decades in the 15th century, the Hermandad de las Marismas, the trading association formed by the ports of Castile along the Cantabrian coast, resembling in some ways the Hanseatic League, fought against the latter, an ally of England, a rival of Castile in political and economic terms.
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