how do the above mentioned hotspots move?
UNANSWERABLE
where is the hot spot that created the hawaiian volcanoes at the moment The Hawai’i hotspot is a volcanic hotspot located near the namesake Hawaiian Islands. what is the temperature recorded at these spots? UNANSWERABLE where are these islands located? North Pacific Ocean. has this island faced any earthquake? On October 15, 2006, there was an earthquake with a magnitude of 6.7 . and what is the weather like here? The climate of the Hawaiian Islands is tropical but it experiences many different climates, depending on altitude and weather. why do the above mentioned natural calamity occur? An earthquake is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. what are its effects? UNANSWERABLE is there any myth linked to it? In Norse mythology, earthquakes were explained as the violent struggling of the god Loki. who is this god? Loki is in some sources the son of Fárbauti and Laufey, and the brother of Helblindi and Býleistr. how did he get his name? The etymology of the name "Loki" has been extensively debated. The name has at times been associated with the Old Norse word "logi" ('flame'). what is the origin of the language you just mentioned? It was a North Germanic language that was spoken by inhabitants of Scandinavia and their overseas settlements.
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Hawaii hotspot [SEP] Wilson's stationary hotspot theory
Wilson proposed that mantle convection produces small, hot buoyant upwellings under the Earth's surface; these thermally active mantle plumes supply magma which in turn sustains long-lasting volcanic activity. This "mid-plate" volcanism builds peaks that rise from relatively featureless sea floor, initially as seamounts and later as fully-fledged volcanic islands. The local tectonic plate (in the case of the Hawaii hotspot, the Pacific Plate) slowly slides over the hotspot, carrying its volcanoes with it without affecting the plume. Over hundreds of thousands of years, the magma supply for the volcano is slowly cut off, eventually going extinct. No longer active enough to overpower erosion, the volcano slowly sinks beneath the waves, becoming a seamount once again.