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Serra da Cangalha is an impact crater in the State of Tocantins, near the border of Maranhão State, in northeastern Brazil. The crater is between 12 and 13 km in diameter, making it the second-largest known crater in Brazil. Its age is estimated to be about 220 million years (Triassic period).〔 The name means ''Pack-Saddle Mountains'' in Portuguese. ==Description== The outer perimeter is a circular inward scarp about 12 km in diameter on the largely undisturbed Cretaceous and upper Silurian sediments of the Parnaíba basin, breached on the west, north, and south sides by drainage valleys. Within the perimeter there is a series of concentric circular valleys and a central basin, all at roughly the same elevation, separated by ring walls. Shuttle Radar Topography Mission imagery shows a faint ring about 11 km in diameter, a second ring of gentle hills about 5–6 km in diameter, and an inner ring of steeper hills, about 3 km in diameter and up to 420 m high, open to the northwest, surrounding a central basin about 2.2 km in diameter.〔(【引用サイトリンク】 author = R. Gregio )〕〔 The impact origin is attested by the presence of impact breccias, quartzite shatter cones and shocked quartz. The meteorite is believed to have struck the surface at a low oblique angle, 25 to 30 degrees on dry land. Radial faults are present inside the crater, and some extend up to 16 km from the center.〔 Disturbed and steeply inclined sediments from the Carboniferous and Devonian periods occur within the crater. A magnetic survey of the structure indicates that deformation within the crater extends to a depth of about 2 km.〔〔 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Serra da Cangalha」の詳細全文を読む スポンサード リンク
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