Hawaii’s Mauna Loa volcano starts to erupt

&Tab;&Tab;<div class&equals;"wpcnt">&NewLine;&Tab;&Tab;&Tab;<div class&equals;"wpa">&NewLine;&Tab;&Tab;&Tab;&Tab;<span class&equals;"wpa-about">Advertisements<&sol;span>&NewLine;&Tab;&Tab;&Tab;&Tab;<div class&equals;"u top&lowbar;amp">&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;<amp-ad width&equals;"300" height&equals;"265"&NewLine;&Tab;&Tab; type&equals;"pubmine"&NewLine;&Tab;&Tab; data-siteid&equals;"111265417"&NewLine;&Tab;&Tab; data-section&equals;"1">&NewLine;&Tab;&Tab;<&sol;amp-ad>&NewLine;&Tab;&Tab;&Tab;&Tab;<&sol;div>&NewLine;&Tab;&Tab;&Tab;<&sol;div>&NewLine;&Tab;&Tab;<&sol;div><p>Hawaii’s Mauna Loa&comma; the world’s largest active volcano&comma; has started to erupt&comma; prompting volcanic ash and debris to fall nearby&period;<&sol;p>&NewLine;<p>The eruption began late on Sunday night in the summit caldera of the volcano on the Big Island&comma; the US Geological Survey said&period;<&sol;p>&NewLine;<p>Early on Monday&comma; it said lava flows were contained within the summit area and were not threatening nearby communities&period;<&sol;p>&NewLine;<p>Officials at the Hawaiian Volcano Observatory said&colon; &OpenCurlyDoubleQuote;Lava flows in the summit region are visible from Kona&period; There is currently no indication of any migration of the eruption into a rift zone&period;”<&sol;p>&NewLine;<p>A rift zone is where the mountain is splitting apart&comma; with the rock cracked and relatively weak&comma; making it is easier for magma to emerge&period;<&sol;p>&NewLine;<p>The agency warned residents at risk from Mauna Loa lava flows should review their eruption preparations&period;<&sol;p>&NewLine;<p>Scientists had been on alert because of a recent spike in earthquakes at the summit of the volcano&comma; which last erupted in 1984&period;<&sol;p>&NewLine;<p>Mauna Loa&comma; rising 13&comma;679 feet &lpar;4&comma;169 metres&rpar; above sea level&comma; is the much larger neighbour to Kilauea volcano&comma; which erupted in a residential neighbourhood and destroyed 700 homes in 2018&period;<&sol;p>&NewLine;<p>Some of its slopes are much steeper than Kilauea’s so when it erupts&comma; its lava can flow much faster&period;<&sol;p>&NewLine;<p>During a 1950 eruption&comma; the mountain’s lava travelled 15 miles &lpar;24 kilometres&rpar; to the ocean in less than three hours&period;<&sol;p>&NewLine;&Tab;&Tab;&Tab;<div style&equals;"padding-bottom&colon;15px&semi;" class&equals;"wordads-tag" data-slot-type&equals;"belowpost">&NewLine;&Tab;&Tab;&Tab;&Tab;<div id&equals;"atatags-dynamic-belowpost-68cd3c8e409c2">&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;<script type&equals;"text&sol;javascript">&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;window&period;getAdSnippetCallback &equals; function &lpar;&rpar; &lbrace;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;if &lpar; false &equals;&equals;&equals; &lpar; window&period;isWatlV1 &quest;&quest; false &rpar; &rpar; &lbrace;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&sol;&sol; Use Aditude scripts&period;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;window&period;tudeMappings &equals; window&period;tudeMappings &vert;&vert; &lbrack;&rsqb;&semi;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;window&period;tudeMappings&period;push&lpar; &lbrace;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;divId&colon; 'atatags-dynamic-belowpost-68cd3c8e409c2'&comma;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;format&colon; 'belowpost'&comma;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&rcub; &rpar;&semi;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&rcub;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&rcub;&NewLine;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;if &lpar; document&period;readyState &equals;&equals;&equals; 'loading' &rpar; &lbrace;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;document&period;addEventListener&lpar; 'DOMContentLoaded'&comma; window&period;getAdSnippetCallback &rpar;&semi;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&rcub; else &lbrace;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;window&period;getAdSnippetCallback&lpar;&rpar;&semi;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;&Tab;&rcub;&NewLine;&Tab;&Tab;&Tab;&Tab;&Tab;<&sol;script>&NewLine;&Tab;&Tab;&Tab;&Tab;<&sol;div>&NewLine;&Tab;&Tab;&Tab;<&sol;div>


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