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Three quivers. A quiver is a container for holding arrows or bolts. It can be carried on an archer's body, the bow, or the ground, depending on the type of shooting and the archer's personal preference. Quivers were traditionally made of leather, wood, furs, and other natural materials, but are now often made of metal or plastic.
Later, M-80s were manufactured as consumer fireworks made from a small cardboard tube, often red, approximately 1 + 1 ⁄ 2 inches (3.8 cm) long and 9 ⁄ 16 inch (1.4 cm) inside diameter, with a fuse coming out of the side; this type of fuse is commonly known as cannon fuse or Visco fuse, after a company responsible for standardizing the product.
Valles Caldera is the younger of two calderas known at this location, having collapsed over and buried the older Toledo Caldera, which in turn may have collapsed over yet older calderas. The associated Cerros del Rio volcanic field , which forms the eastern Pajarito Plateau and the Caja del Rio , is older than the Toledo Caldera.
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A BLU-82B bomb with a daisy cutter, used by the United States Air Force. A daisy cutter is a type of fuse designed to detonate an aerial bomb at or above ground level. The fuse itself is a long probe affixed to the weapon's nose, which detonates the bomb if it touches the ground or any solid object.
Smallfoot was first proposed in 2001. The name Smallfoot (whilst trademarked by SCO) was never the intended product's final name, but rather was a working name that stuck. A first prototype was built around the Linux platform. A deal was signed in January 2003 for Smallfoot to work on Beetle point-of-sale terminals from Wincor Nixdorf. [4]
Yebira, Ebira and Shiko (箙, lit. the "[Japanese] Quiver (of Arrows)") are types of quiver used in Japanese archery. The quiver is unusual in that in some cases, it may have open sides, while the arrows are held in the quiver by the tips which sit on a rest at the base of the ebira, and a rib that composes the upper part and keeps them in place.
The zircon and phenocrysts rims recorded that the magma of the Lava Creek Tuff was generated from a mix of mantle, Archean crust, and shallow hydrothermally altered intra-caldera rocks. Member A and B were sourced from separate magma reservoirs prior to eruption, [ 19 ] at a depth range of 3–6 km (1.9–3.7 mi) [ 20 ] and a temperature of 790 ...