Since the Hawaiian Islands were all created by volcanic activity, it is somewhat surprising that only the island of Hawaii now possesses any active volcanoes. Why did the volcanoes that built the other islands stop erupting and why are those on the big island still active? This video segment, adapted from a NOVA television broadcast, shows how plumes of hot material rise from the Earth's interior to create 'hot spots' in the crust which are the locations of volcanic activity. Movement of the Pacific Plate causes volcanic islands to continually form, migrate away from the hot spot, and become extinct, forming chains of islands like the Hawaiian Islands. The segment is four minutes thirty-seven seconds in length. Educational levels: High scho...
Bathymetry and the geoid anomaly of the northern flank of the Hawaiian swell is broader and higher t...
Hawaiian volcanoes are formed by the eruption of large quantities of basaltic magma related to hot- ...
Mantle plumes are buoyant upwellings of hot rock that transport heat from Earth's core to its surfac...
Destructive, deadly, and able to uproot and ruin lives, yet awe inspiring and a supportive platform ...
Hot spot theory provides a key framework for understanding the motion of the tectonic plates, mantle...
This lesson provides students with information about how islands are formed, including a basic knowl...
I he island of Hawaii and the other islands of the Hawaiian chain are prod-ucts of volcanic eruption...
This lesson introduces the idea that rates and directions of plate movements can be measured. The di...
What causes volcanoes? What role do they play in the formation and maintenance of our planet? And is...
Ocean islands, seamounts and volcanic ridges are thought to form above mantle plumes. Yet, this mech...
The Hawaiian-Emperor volcanic chain stretches nearly 6,000 km across the North Pacific Ocean and con...
In this lesson students investigate the formation of the Hawaiian archipelago to see what geological...
Intraplate or "hot spot" volcanic island chains, exemplified by Hawaii, play an important role in pl...
This site describes where volcanoes are found in terms of plate tectonics and explains why they occu...
Volcanic settings vary widely not only in their eruptive style and products, but in the manner magma...
Bathymetry and the geoid anomaly of the northern flank of the Hawaiian swell is broader and higher t...
Hawaiian volcanoes are formed by the eruption of large quantities of basaltic magma related to hot- ...
Mantle plumes are buoyant upwellings of hot rock that transport heat from Earth's core to its surfac...
Destructive, deadly, and able to uproot and ruin lives, yet awe inspiring and a supportive platform ...
Hot spot theory provides a key framework for understanding the motion of the tectonic plates, mantle...
This lesson provides students with information about how islands are formed, including a basic knowl...
I he island of Hawaii and the other islands of the Hawaiian chain are prod-ucts of volcanic eruption...
This lesson introduces the idea that rates and directions of plate movements can be measured. The di...
What causes volcanoes? What role do they play in the formation and maintenance of our planet? And is...
Ocean islands, seamounts and volcanic ridges are thought to form above mantle plumes. Yet, this mech...
The Hawaiian-Emperor volcanic chain stretches nearly 6,000 km across the North Pacific Ocean and con...
In this lesson students investigate the formation of the Hawaiian archipelago to see what geological...
Intraplate or "hot spot" volcanic island chains, exemplified by Hawaii, play an important role in pl...
This site describes where volcanoes are found in terms of plate tectonics and explains why they occu...
Volcanic settings vary widely not only in their eruptive style and products, but in the manner magma...
Bathymetry and the geoid anomaly of the northern flank of the Hawaiian swell is broader and higher t...
Hawaiian volcanoes are formed by the eruption of large quantities of basaltic magma related to hot- ...
Mantle plumes are buoyant upwellings of hot rock that transport heat from Earth's core to its surfac...