Davidof Volcano facts for kids
Quick facts for kids Davidof Volcano |
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Highest point | |
Elevation | 1,050 ft (320 m) |
Geography | |
Location | North Pacific, part of Alaska |
Parent range | Aleutian Islands |
Geology | |
Age of rock | Cenozoic |
Mountain type | Stratovolcano |
Volcanic arc/belt | Aleutian Arc |
Davidof Volcano is an inactive stratovolcano (a cone-shaped volcano) located in the Aleutian Islands of Alaska, USA. It's about 1,991 kilometers (1,237 miles) from Anchorage. This volcano sits on Davidof Island, which is part of the Rat Islands. Davidof Volcano is also part of a special group of four islands called the "Aleutian Krakatau." These islands were formed a long time ago when a large volcano's top collapsed.
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Visiting Davidof Island
Davidof Island has no people living on it. This means it's quite hard to get there. The closest town with transportation options is Adak. However, Adak is still about 320 kilometers (199 miles) away from Davidof Island.
What is Davidof Volcano like?
Davidof Volcano is a stratovolcano. This type of volcano has steep sides and is built up from many layers of hardened lava and ash. Davidof is actually what's left of a much bigger volcano. Its top likely collapsed at the end of the Cenozoic period, which was a very long time ago.
The part of the volcano that collapsed now forms a "caldera." This caldera stretches about 80 meters (262 feet) underwater. Davidof Island has a unique shape with many steep cliffs. You won't find any visible rivers or lakes on the island.
What is Davidof Volcano made of?
Scientists don't know the exact makeup of Davidof Volcano. But studies show that its lava layers sit on top of a base of red breccia. Breccia is a rock made of broken pieces of minerals or rocks.
The lava itself is mostly gray. It can be either glassy or fine-grained. The lava and ash layers on Davidof overlap each other. The very top layer is made of pyroclastic flow deposits. These are fast-moving currents of hot gas and volcanic rock.
The lava also contains tiny crystals called phenocrysts. These crystals include feldspar, olivine, and pyroxene. You can easily find them in the lava areas.
Has Davidof Volcano erupted?
No eruptions from Davidof Volcano have ever been recorded by people. However, there is proof that the volcano was active in the past. Pictures taken from the air show lava flow deposits on the sides of the island. Scientists believe these lava flows are probably less than 10,000 years old.
Animals and Plants on Davidof Island
Even though Davidof Island is small, it has a lot of plants. You can find different types of moss, lichen, and heath plants. Grass and sedge plants cover much of the lower parts of the island.
Other plants like fungi, liverworts, horsetails, and ferns also grow there. There are also many flowering plants. These include the narcissus anemone, lupines, and orchids. Seaweed is also very common on the island's beaches.