"Due to unjointed laws and basic incompetence of the government, the US has suffered a self-inflicted wound in the murder of our daughter by the hand of a person that should have never been on the streets in this country," he said.
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Hoplopteryx has a dorsal fin supported by nine unjointed, bony rays, deeply forked, homocercal tail, a moderately developed anal fin, and a pelvic fin located well forward. The snout is quite short, the eyes fairly large, and both jaws of the upturned mouth hold small teeth.
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This increases the curb effect, especially when the rein is placed on the lower of the two slots. Kimblewick bits have a variety of bit mouthpieces. The original design has a ported mouthpiece, but it now is also manufactured with others, including a solid, unjointed "mullen" mouth, and a single-jointed mouthpiece.
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Retrieving a dead mob member's knife, George Marlow unjointed his dead brother' ankles. He and Charlie used a wagon to escape the ambush site. Three members of the mob were also killed and a number of others wounded. Several members of the mob were later prosecuted and convicted for the assault upon the brothers.
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K. pilae are roundish-oval mites. The males are up to 220 µm long and about 150 µm wide, females up to 356 µm long and about 300 µm wide. The four pairs of legs are short and stubby in shape and have five segments. At the ends of the extremities, males have unjointed grippers and suckers, while females have claws.
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A geologic map of Yosemite National Park El Capitan Granite is a type of granite (also see granodiorite), in a large area near El Capitan, in Yosemite National Park, California, United States. The granite forms part of the Tuolumne Intrusive Suite (also known as Tuolumne Batholith), one of the four major intrusive suites within the Sierra Nevada. El Capitan granite is mostly unjointed.
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The exterior walls of the Carolingian octagon, made of quarry stone, is largely unjointed and lacks further ornamentation. The only exception is that the projections of the pillars of the cupola are crowned by antique capitals. Above the Carolingian masonry, there is a Romanesque series of arches above a late Roman gable. The Octagon is crowned by unusual baroque vents.
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The great majority of Yosemite Valley's widening, for example, was due to joint- controlled rockfall. In fact, only 10% of its widening and 12% of its excavation are thought to be the result of glaciation. Large, relatively unjointed volumes of granite form domes such as Half Dome and monoliths like the high El Capitan. Closely spaced joints lead to the creation of columns, pillers, and pinnacles such as Washington Column, Cathedral Spires, and Split Pinnacle.
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Together, they form a barrier on the north side of the mouth of Little Yosemite Valley. Both Liberty Cap and Mount Broderick are roches moutonnées, features that protruded above or resisting being overridden by successive Merced River glaciers because they are made of massive unjointed granite sufficiently resistant to glacial erosive power, leaving them prominent in the post-glacial landscape. Both features are glacially polished on their glacier-facing side and ragged on their leeward side.
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Hence annelids' chetae are structurally different from the setae ("bristles") of arthropods, which are made of the more rigid α-chitin, have a single internal cavity, and are mounted on flexible joints in shallow pits in the cuticle. Nearly all polychaetes have parapodia that function as limbs, while other major annelid groups lack them. Parapodia are unjointed paired extensions of the body wall, and their muscles are derived from the circular muscles of the body. They are often supported internally by one or more large, thick chetae.
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Manglors was a line of action figures originally released by the Ideal Toy Company in 1984-85 and re-licensed by Toyfinity in 2013.Welcome to Toyfinity The first wave consisted of Manglord (which was initially released with a playset Manglor Mountain), Manglosaurus and Manglodactyl. A second wave, packaged with plastic eggs, appeared in 1985, which included Manglodemon, Manglizard, and Manglodragon. The line consisted of flexible, unjointed (one piece), sticky, and mostly unpainted (some versions of Manglord had purple highlights) Sorbothane figures that were not able to stand on their own.
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This rearward weight distribution encouraged planing, but could lead to some peculiar attitudes when setting off at slow speeds, as the whole boat appeared to be sinking by the stern. The displacement was only and the engine alone weighed . Construction was of plywood, although the attention paid to weight-saving was such that this was laminated to order from varying numbers of veneers, rather than sawn from factory-made standard sheets. The frames are formed of single-piece unjointed sheets of 7-ply, the hull skins of 5-ply and the deck of 6-ply.
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Below this are two layers of muscles, which develop from the lining of the coelom (body cavity): circular muscles make a segment longer and slimmer when they contract, while under them are longitudinal muscles, usually four distinct strips, whose contractions make the segment shorter and fatter. Some annelids also have oblique internal muscles that connect the underside of the body to each side. The setae ("hairs") of annelids project out from the epidermis to provide traction and other capabilities. The simplest are unjointed and form paired bundles near the top and bottom of each side of each segment.
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Pioneer Design Studio and Monash University, Melbourne. Mammalodon fossils have been found in Australia and New Zealand Mammalodon was, at first, considered to be a member of Archaeoceti, an ancient group of whales, which was evidenced by its apparent ancient features, such as the variety of differently shaped teeth in its jaw (heterodonty) that modern whales lack. Mammalodon was first considered to be a baleen whale in a 1982 study despite having no baleen; instead, they cited other similarities such as loosely sutured bones in the snout, a broad and flat roof of the mouth, and an unjointed mandibular symphysis between the two halves of the jawbone. It belongs to the family Mammalodontidae, along with Janjucetus.
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Cascade Cliffs is a wall of unjointed granite that rises to AMSL, above the Merced River and make up the southern wall of Little Yosemite Valley at , southwest of Bunnell Point and northeast of Mount Starr King, of which Cascade Cliffs comprises the northern flank. In few other places in the Yosemite region is the granite more continuously massive than in the Cascade Cliffs. Only one horizontal master joint divides the rock (in the lower left) The scales on the cliffs are merely surficial features due to exfoliation. The dark streaks indicate the paths followed by the ribbon cascades which descend from the upland in the spring, when the snow is melting, and from which the cliffs take their name.
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The first Burgess Shale fossils were found on Mount Stephen in Canada's Rocky Mountains by a construction worker, whose reports of them reached Richard McConnell of the Geological Survey of Canada. McConnell found trilobite beds there in 1886, and some unusual fossils that he reported to his superior. These were misdiagnosed as headless shrimps with unjointed appendages, and were named Anomalocaris because of their unusual appendages – but turned out to be pieces of a puzzle that took 90 years to solve. Charles Walcott searches the Burgess Shale for fossils, assisted by his wife and son, c. 1913 Similar fossils were reported in 1902 from nearby Mount Field, another part of the Stephen formation. These may have been why Charles Doolittle Walcott visited Mount Field in 1909.
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The radiating brackets and blocks that support the deep eaves of the roof are "cloud-shaped" (), a type found only in the earliest buildings to survive to the modern period: the kondō, pagoda, and central gate (chūmon) at Hōryū-ji, and the three-storey pagodas at Hokki-ji and Hōrin-ji (the last was struck by lightning and burnt to the ground in 1944). The bracket system supports that extend far into the eaves. In a full-scale building, the downward load of the eaves upon the far end of these tail rafters is counterbalanced at the other end by the main load of the roof. The simple unjointed purlins that support the roof covering in the eaves are circular in cross-section, as opposed to the rectangular purlins of the earliest surviving buildings.
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North Wall of Little Yosemite Valley The north wall of Little Yosemite has not been subject to the same kinds of glacial planing as the south wall because the granite rocks of Moraine Dome and Sugar Bowl Dome are tougher and more resistant. This is remarkable considering that it is likely that Little Yosemite was not only scoured repeatedly by glaciers that were wholly contained by the canyon, but also overrun by glaciers that overflowed the Merced canyon and spread widely into surrounding uplands with occasional surges of ice contributed over the pass from the overflowing Tuolumne River basin. These rocks were thus subject to tremendous gravitational and flow forces yet retain a remarkable degree of integrity, eroding almost exclusively and superficially along exfoliation joints. The south wall of the valley has been subject to extensive glacial planing, with all jointed granite completely smoothed away, leaving a stark, featureless unjointed sheer cliff face, as is apparent in the image of Little Yosemite Valley from Washburn Point, above right.
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