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The Type 3 Chi-Nu medium tank retained the same hull and suspension of the Type 1 Chi-He, with the addition of an enlarged turret ring for the new large hexagonal gun turret with a commander's cupola. [2] [15] The more powerful main armament, a Type 3 75 mm tank gun, was based on the Japanese Type 90 field gun. [16]
The tendency of felsic lava to be cooler than mafic lava increases the viscosity difference. The silicon ion is small and highly charged, and so it has a strong tendency to coordinate with four oxygen ions, which form a tetrahedral arrangement around the much smaller silicon ion. This is called a silica tetrahedron. In a magma that is low in ...
The Tibesti Mountains are a mountain range in the central Sahara, primarily located in the extreme north of Chad, with a small portion located in southern Libya.The highest peak in the range, Emi Koussi, lies to the south at a height of 3,415 meters (11,204 ft) and is the highest point in both Chad and the Sahara.
The round is a 105 mm (4.1 in) tandem shaped charge with a weight of 10.3 kg (23 lb) and has a range of 200 m (660 ft) and a stated penetration capability in excess of 600 mm (24 in) rolled homogeneous armor (RHA) (after ERA), 1,500 mm (59 in) reinforced concrete, 2,000 mm (79 in), and 3,700 mm (150 in) of soil. [18]
Pillow lava on the ocean floor of Hawaii. Pillow lavas are lavas that contain characteristic pillow-shaped structures that are attributed to the extrusion of the lava underwater, or subaqueous extrusion. Pillow lavas in volcanic rock are characterized by thick sequences of discontinuous pillow-shaped masses, commonly up to one meter in diameter.
Some lava flows hold a mixture of multilevel and multilateral tubes. One other form a lava tube can take is the tube-in-tube which can form inside lava tubes if the linings of the walls are weak enough to lean inward, forming a new floor above the old. Tube-in-tubes are generally noted to form during the last lava draining through the main lava ...
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