No. While volcanoes can erupt very hot material, a volcano that is not actively erupting may not be any warmer than an ordinary mountain. Even on an active volcano, temperatures away from the vent may be normal.
flood basalts and volcanoes
Hot spots have generated all types of volcanoes but are most often. If you mean to ask about specific volcanoes, there are too many to count, so a few groups and notable volcanoes will be listed: The volcanoes of Hawaii The volcanoes of the Canary Islands The Yellowstone supervolcano The San Francisco volcanic complex (including Sunset Crater and the San Francisco Peaks) The volcanoes of Iceland (associated with both a hot spot and a divergent plate boundary).
No. Hot spots and subduction zones are two separate geogolgic settings in which volcanoes can form. Some hot spots may develop as a result of activity in a subduction zone, and continue activity after subduction has ended or move away.
Shield volcanoes typically form on hot spots. These volcanoes have gentle slopes due to the low-viscosity basaltic lava they produce. Examples of shield volcanoes formed on hot spots include Mauna Loa in Hawaii and Galapagos Islands in Ecuador.
Yes I am pretty sure.
Shield volcanoes are not hot spots but they are associated with them. However, such volcanoes can also form at rift zones.
Yes, it is not uncommon to find volcanoes at hot spots.
flood basalts and volcanoes
Which volcanoes are located at hot spots
flood basalts and volcanoes
at hot spots(a place where volcanoes are very active)
Which volcanoes are located at hot spots
Hot spots have generated all types of volcanoes but are most often. If you mean to ask about specific volcanoes, there are too many to count, so a few groups and notable volcanoes will be listed: The volcanoes of Hawaii The volcanoes of the Canary Islands The Yellowstone supervolcano The San Francisco volcanic complex (including Sunset Crater and the San Francisco Peaks) The volcanoes of Iceland (associated with both a hot spot and a divergent plate boundary).
No. Hot spots and subduction zones are two separate geogolgic settings in which volcanoes can form. Some hot spots may develop as a result of activity in a subduction zone, and continue activity after subduction has ended or move away.
no hot spots
Shield volcanoes typically form on hot spots. These volcanoes have gentle slopes due to the low-viscosity basaltic lava they produce. Examples of shield volcanoes formed on hot spots include Mauna Loa in Hawaii and Galapagos Islands in Ecuador.
Volcanoes form from either techtonic plates crashing together or from hot spots under the earth