The term crony capitalism made a significant impact in the public arena as an explanation of the Asian financial crisis.
Hawaiian eruptions may occur along fissure vents, such as during the eruption of Mauna Loa Volcano in 1950, or at a central vent, such as during the 1959 eruption in KÄ«lauea Iki Crater, which created a lava fountain 580 meters (1,900 ft) high and formed a 38-meter cone named Pu Ê» u Pua Ê» i.ery little amounts of volcanic ash are produced. This type of eruption occurs most often at hotspot volcanoes such as KÄ«lauea and Iceland, though it can occur near subduction zones (e.g. Medicine Lake Volcano in California, United States) and rift zones.
Hawaiian eruptions are a type of volcanic eruption, named after the Hawaiian volcanoes with which this eruptive type is hallmark. Hawaiian eruptions are the calmest types of volcanic events, characterized by the effusive eruption of very fluid basalt-type lavas with low gaseous content. Two years into its life, pyroclastic activity began to wane, and the outpouring of lava from its base became its primary mode of activity. 2  Eruptions ceased in 1952, and the final height was 424 m (1,391 ft). 3  This was the first time that scientists are able to observe the complete life cycle of a volcano.