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・ Lateral costotransverse ligament
・ Lateral cricoarytenoid muscle
・ Lateral cutaneous branch
・ Lateral cutaneous branch of iliohypogastric nerve
・ Lateral cutaneous nerve
・ Lateral cutaneous nerve of arm
・ Lateral cutaneous nerve of forearm
・ Lateral cutaneous nerve of thigh
・ Lateral dorsal cutaneous nerve
・ Lateral dorsal nucleus of thalamus
・ Lateral earth pressure
・ Lateral electrical surface stimulation
・ Lateral epicondyle
・ Lateral epicondyle of the femur
・ Lateral epicondyle of the humerus
Lateral eruption
・ Lateral expansion
・ Lateral flap
・ Lateral flow test
・ Lateral force variation
・ Lateral funiculus
・ Lateral genicular artery
・ Lateral geniculate nucleus
・ Lateral giant interneuron
・ Lateral globus pallidus
・ Lateral grey column
・ Lateral horn
・ Lateral horn of insect brain
・ Lateral hypothalamus
・ Lateral inguinal fossa


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Lateral eruption : ウィキペディア英語版
Lateral eruption
A lateral eruption, also called a flank eruption or lateral blast if explosive, is a volcanic eruption that takes place on the flanks of a volcano instead of at the summit. Lateral eruptions are typical at rift zones where a volcano is breaking apart. Since it is easier for molten rock to flow laterally out the sides of weak flanks, the flank gives way before magma is pushed up through a conduit that feeds magma to the summit. These features are commonly found at shield volcanoes and produce basaltic lava flows and cinder cones.
Lateral blasts are understood to be created by immediate decompression of a magma chamber lying not far below the flanks of a volcano, similar to what occurred during the 1980 eruption of Mount St. Helens in the U.S. state of Washington, or along the base or flanks of a lava dome similar to what happened during the 1902 eruption of Mount Pelée
on the northern tip of the French overseas department of Martinique in the Lesser Antilles island arc of the Caribbean.
==References==


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「Lateral eruption」の詳細全文を読む



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