Share & grow the world's knowledge!
We want to connect the people who have knowledge to the people who need it, to bring together people with different perspectives so they can understand each other better, and to empower everyone to share their knowledge.
Which of the following is not an extinct volcano? (A) Mauna Loa (B) Demavand (C) Chimborazo (D) Koh-i-Sultan
Mauna Loa is an active shield volcano located in Hawaii and is the largest subaerial volcano on our planet. It is part of the Hawaiian hotspot chain and has erupted thirty-four times since its first well-documented eruption in 1843. This high frequency of activity contrasts sharply with extinct volcRead more
Mauna Loa is an active shield volcano located in Hawaii and is the largest subaerial volcano on our planet. It is part of the Hawaiian hotspot chain and has erupted thirty-four times since its first well-documented eruption in 1843. This high frequency of activity contrasts sharply with extinct volcanoes like Demavand or Chimborazo. Extinct volcanoes have no magma supply and are unlikely to erupt again over geological timescales. Mauna Loa’s frequent basaltic lava flows and monitored seismic activity confirm it is very much alive, making it a critical site for global volcanic research and hazard monitoring.
See lessThe correct ascending order of types of volcanoes based on the intensity of eruption is:
Volcanic eruptions are classified by their violence and the viscosity of their magma. Hawaiian eruptions are the least intense, producing fluid basaltic lava flows. Strombolian eruptions follow, involving moderate bursts of glowing cinders. Vulcanian eruptions are significantly more powerful, launchRead more
Volcanic eruptions are classified by their violence and the viscosity of their magma. Hawaiian eruptions are the least intense, producing fluid basaltic lava flows. Strombolian eruptions follow, involving moderate bursts of glowing cinders. Vulcanian eruptions are significantly more powerful, launching dark, ash-laden clouds and solid rock fragments. At the peak of intensity is the Pelean type, named after Mount Pelée. These are characterized by extremely thick magma that traps gases until they explode, generating nuées ardentes or pyroclastic flows. This scale helps seismologists categorize the danger levels associated with different volcanic structures and their specific tectonic settings.
See lessWhere is the Valley of Ten Thousand Smokes found?
The Valley of Ten Thousand Smokes is a spectacular volcanic landscape in Alaska, USA. It was created following the 1912 eruption of Novarupta, which deposited ash flows up to 700 feet deep across the region. As surface water filtered down into the hot ash, it turned into steam, emerging through thouRead more
The Valley of Ten Thousand Smokes is a spectacular volcanic landscape in Alaska, USA. It was created following the 1912 eruption of Novarupta, which deposited ash flows up to 700 feet deep across the region. As surface water filtered down into the hot ash, it turned into steam, emerging through thousands of fumaroles. Botanist Robert Griggs discovered the valley in 1916 and gave it its descriptive name. While most of these steam vents have since vanished as the ash cooled, the area remains a vital location for geologists studying ignimbrite deposits and explosive volcanic history.
See lessWhich of the following types of volcanoes has a cauliflower-like shape? (A) Strombolian type (B) Hawaiian type (C) Vulcanian type (D) Pelean type
Vulcanian eruptions are named after the island of Vulcano in Italy. They occur when sticky magma clogs the vent, causing gas pressure to build until it explodes. The hallmark of this eruption is the massive eruption column that looks like a giant cauliflower. This billowing effect happens as the hotRead more
Vulcanian eruptions are named after the island of Vulcano in Italy. They occur when sticky magma clogs the vent, causing gas pressure to build until it explodes. The hallmark of this eruption is the massive eruption column that looks like a giant cauliflower. This billowing effect happens as the hot, ash-heavy gas surges upward and expands rapidly in all directions. These clouds can reach altitudes of several kilometers and carry large volcanic bombs. The cauliflower appearance is a result of the high-velocity turbulence within the cloud, which carries fine ash and dust across large distances.
See lessWhich of the following types of volcanoes is also called a Pelean type volcano?
In many historical geography contexts, the Vesuvian type is categorized alongside the Pelean type because both represent the most violent end of the volcanic spectrum. Named after the 79 AD eruption of Mount Vesuvius, these eruptions are characterized by sustained, high-altitude eruption columns thaRead more
In many historical geography contexts, the Vesuvian type is categorized alongside the Pelean type because both represent the most violent end of the volcanic spectrum. Named after the 79 AD eruption of Mount Vesuvius, these eruptions are characterized by sustained, high-altitude eruption columns that spread ash across thousands of square miles. Both types rely on gas-rich, high-viscosity magma. While the Pelean type is famous for its horizontal pyroclastic flows, the Vesuvian type is noted for its vertical power. They are often grouped together when discussing the mechanics of silica-rich, explosive eruptions that drastically alter global climates and landscapes.
See less