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The Hawaiian volcanoes come from a hot spot whereas the ring of fire volcanoes are from subduction zones. A hot spot is an area that was thought to be a relatively stationary plume of hot rock coming up from deep in the Earth's mantle. As the Earth's crust passes over the hot spot, the plume burns through it, creating volcanoes. Recent research shows that rather than being relatively stationary, these hot spots actually do move. How they move is a subject of current research.
Subduction zone volcanoes come from the melting of the down-going plate.
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What is the name for the hawaiian volcano goddess?
The Hawaiian volcano goddess is known as Pele. She is considered a powerful and passionate deity associated with fire, lightning, wind, and volcanoes in Hawaiian mythology.
Who is the goddess Pele?
Pele is the Hawaiian goddess of fire, lightning, wind, and volcanoes. She is seen as a powerful and capricious deity, with legends attributing volcanic eruptions to her anger or displeasure. Pele is also revered as the creator of the Hawaiian islands.
Are hawaiian islands cinder cone volcanoes?
The Hawaiian volcanoes can form cinder cones, however the type of volcano they are classified as is shield volcano due to their broad sloping sides and the ability for their lava to flow.No. The Hawaiian islands are shield volcanoes.
Are there shield volcanoes in the ring of fire?
Yes, there are shield volcanoes in the Ring of Fire. Shield volcanoes are common along tectonic plate boundaries, including those found in the Ring of Fire, such as in Hawaii and the Pacific Northwest. These volcanoes are characterized by their broad, gently sloping sides and can produce both effusive and explosive eruptions.
What are the volcanoes on the edges of the Pacific plate called?
Volcanoes on the edges of the Pacific plate are often referred to as "Ring of Fire" volcanoes. This is due to their location around the Pacific Plate's boundaries, where tectonic activity leads to frequent volcanic eruptions.
What is the difference between Hawaiian volcanoes and those of the Ring of Fire?
The Pacific Ring of Fire literally surrounds the basin of the Pacific Ocean, whereas the Hawaiian volcanoes are the result of the Hawaiian hotspot.See the related Wikipedia links for pictures and more information:
Who was mt Pelee named after?
the Hawaiian goddess of fire/volcanoes, Pele.
Are the volcanoes of the Hawaiian Islands part of the Pacific Ring of Fire Boundary?
yes they are!!
Who is god Pele associated with?
Pele is actually a Hawaiian goddess associated with volcanoes and fire.
What is the name for the hawaiian volcano goddess?
The Hawaiian volcano goddess is known as Pele. She is considered a powerful and passionate deity associated with fire, lightning, wind, and volcanoes in Hawaiian mythology.
What is pel'e?
Pele' is either the Hawaiian goddess of fire (volcanoes), or the name of a phenomenal former pro soccer player.
Who is the goddess Pele?
Pele is the Hawaiian goddess of fire, lightning, wind, and volcanoes. She is seen as a powerful and capricious deity, with legends attributing volcanic eruptions to her anger or displeasure. Pele is also revered as the creator of the Hawaiian islands.
Are hawaiian islands cinder cone volcanoes?
The Hawaiian volcanoes can form cinder cones, however the type of volcano they are classified as is shield volcano due to their broad sloping sides and the ability for their lava to flow.No. The Hawaiian islands are shield volcanoes.
What is the hawaiian word for fire?
Fire in Hawaiian is pronounced Ahi
Why do the hawaiian islands get smaller when they move northwest?
The Hawaiian islands are made from volcanic eruptions. The active volcanoes in the circle of fire are to the south of Hawaii.
What is the Hawaiian translation for fire?
The Hawaiian translation for fire is Ahi, spoken as AH-he.
Are there shield volcanoes in the ring of fire?
Yes, there are shield volcanoes in the Ring of Fire. Shield volcanoes are common along tectonic plate boundaries, including those found in the Ring of Fire, such as in Hawaii and the Pacific Northwest. These volcanoes are characterized by their broad, gently sloping sides and can produce both effusive and explosive eruptions.
