Rhyolitic
Pāhoehoe lava flows most like dripping wax. Pāhoehoe is a type of basaltic lava that has a low viscosity, giving it a smooth and ropy appearance as it flows. This type of lava can form various features, including smooth channels and dripping formations that resemble dripping wax.
Kilauea produces a'a and pahoehoe lava flows.
Yellowstone has produced both basaltic and rhyolitic lava flows. It is better known for its ecplosive eruptions, which produce large ash clouds and pyroclastic flows rather than lava flows.
The Mayon Volcano in the Philippines typically has basaltic andesite lava flows, which are characterized by their high silica content and intermediate viscosity, allowing for slow-moving lava flows. This type of lava results in cone-shaped volcanoes with steep slopes.
Basaltic lava is fluid and flows freely from volcanoes due to its low viscosity. This type of lava typically results in gentle, non-explosive eruptions and can travel long distances from the vent.
No. The fastest lava flows on earth have been recorded at Mount Nyiragongo in the Congo flowing at 60 mph (100 km/h). In most cases, however, lava flows very slowly. Blocky lava flows are the slowest, moving at speeds comparable to glaciers.
Basic lava.
basaltic-andesitic
its called "aa''
Pāhoehoe lava flows most like dripping wax. Pāhoehoe is a type of basaltic lava that has a low viscosity, giving it a smooth and ropy appearance as it flows. This type of lava can form various features, including smooth channels and dripping formations that resemble dripping wax.
Kilauea produces a'a and pahoehoe lava flows.
Pahoehoe
Pahoehoe
Yellowstone has produced both basaltic and rhyolitic lava flows. It is better known for its ecplosive eruptions, which produce large ash clouds and pyroclastic flows rather than lava flows.
The type of lava that flows from poas is color purple and it has hot pink streaks from the inner core. The lava is hot...
The Mayon Volcano in the Philippines typically has basaltic andesite lava flows, which are characterized by their high silica content and intermediate viscosity, allowing for slow-moving lava flows. This type of lava results in cone-shaped volcanoes with steep slopes.
stratovolcano