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Mount Tambora formed as a result of a subduction zone. Here, a section of the ocean floor that is part of the Indo-Australian Plate is sliding under part of the Eurasian Plate and into the mantle. The oceanic crust takes some water and other volatiles with it. This seeps into the superheated rock of the mantle, allowing it to melt. It then rises toward the surface and through the crust via cracks. This then emerges on the surface, forming volcanoes such as Mount Tambora.
Some major volcanic eruptions in the Ring of Fire region include the 1815 eruption of Mount Tambora in Indonesia, the 1991 eruption of Mount Pinatubo in the Philippines, and the ongoing activity of Kilauea in Hawaii. These eruptions have had significant impacts on local communities and the environment.
Mount Tambora is a stratovolcano located on the island of Sumbawa in Indonesia. It has a large caldera measuring about 6 km in diameter and 1,000 meters deep, resulting from the volcanic eruption in 1815. The volcano has a prominent summit crater that is still active and has had numerous eruptions throughout history.
Some of the most famous volcanoes include Mount Vesuvius, which destroyed Pompeii and Krakatoa. Mount St. Helens, Mount Tambora, Mauna Loa, and Mount Pelee are also on the list.
Mount Tambora is classified as an active volcano. Although it last erupted in 1815, resulting in the largest eruption in recorded history, it is still considered active because it has the potential to erupt again in the future.
Mount Everest
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· Mount Pele, Martinique · Mount Pinatubo, Philippines · Mount St. Helens, United States · Mount Tambora, Indonesia · Mount Vesuvius, Italy
Mount Berongou
High rugged landforms are also called mountains. There are mountains in virtually every region of the world. Some famous mountains include Mount Everest, Mount Kilimanjaro, and Mount Blanc.
Mount Saint Helens, The Grand Canyon, and Mount Everest are all famous landforms in the US. Another famous landform is the Great Lakes.
Mount Tambora formed as a result of a subduction zone. Here, a section of the ocean floor that is part of the Indo-Australian Plate is sliding under part of the Eurasian Plate and into the mantle. The oceanic crust takes some water and other volatiles with it. This seeps into the superheated rock of the mantle, allowing it to melt. It then rises toward the surface and through the crust via cracks. This then emerges on the surface, forming volcanoes such as Mount Tambora.
Some landforms are flat and some are raised areas because it is created by nature and it is not manmade .
Some major volcanic eruptions in the Ring of Fire region include the 1815 eruption of Mount Tambora in Indonesia, the 1991 eruption of Mount Pinatubo in the Philippines, and the ongoing activity of Kilauea in Hawaii. These eruptions have had significant impacts on local communities and the environment.
A plateau
Mount Tambora is a stratovolcano located on the island of Sumbawa in Indonesia. It has a large caldera measuring about 6 km in diameter and 1,000 meters deep, resulting from the volcanic eruption in 1815. The volcano has a prominent summit crater that is still active and has had numerous eruptions throughout history.
Some of the most famous volcanoes include Mount Vesuvius, which destroyed Pompeii and Krakatoa. Mount St. Helens, Mount Tambora, Mauna Loa, and Mount Pelee are also on the list.