granite fio
A basaltic lava eruption that is low in silica tends to produce effusive eruptions. These eruptions are characterized by relatively gentle and steady flows of lava, rather than explosive eruptions with ash and pyroclastic material. Basaltic lava flows easily due to its low viscosity, allowing it to travel long distances before cooling.
when some people think of volcanic eruptions, they often imagine rivers of red-hot lava, called lava flows. lava flows come from nonexplosive eruptions. it still spurts lava but non-explosivley!
During a nonexplosive eruption, lava flows out from the volcano in a slow and steady manner. The lava is typically less viscous, allowing it to flow smoothly and cover greater distances. This type of eruption is characterized by the slow-moving streams of lava that can create new land formations as they cool and solidify.
During a nonexplosive eruption, you can expect to see a steady flow of lava mainly from fissures or vents on the volcano. This type of eruption typically causes slow-moving lava flows, rather than dramatic explosions. Ash and gas emissions may still occur but are usually not as intense as in explosive eruptions.
A shield volcano forms when layers of basaltic lava accumulate during a nonexplosive eruption. These volcanoes have gentle sloping sides and are usually characterized by their broad and flat shapes. Mauna Loa in Hawaii is a well-known example of a shield volcano.
granite fio
A basaltic lava eruption that is low in silica tends to produce effusive eruptions. These eruptions are characterized by relatively gentle and steady flows of lava, rather than explosive eruptions with ash and pyroclastic material. Basaltic lava flows easily due to its low viscosity, allowing it to travel long distances before cooling.
my buttcheeks
when some people think of volcanic eruptions, they often imagine rivers of red-hot lava, called lava flows. lava flows come from nonexplosive eruptions. it still spurts lava but non-explosivley!
During a nonexplosive eruption, lava flows out from the volcano in a slow and steady manner. The lava is typically less viscous, allowing it to flow smoothly and cover greater distances. This type of eruption is characterized by the slow-moving streams of lava that can create new land formations as they cool and solidify.
During a nonexplosive eruption, you can expect to see a steady flow of lava mainly from fissures or vents on the volcano. This type of eruption typically causes slow-moving lava flows, rather than dramatic explosions. Ash and gas emissions may still occur but are usually not as intense as in explosive eruptions.
A shield volcano forms when layers of basaltic lava accumulate during a nonexplosive eruption. These volcanoes have gentle sloping sides and are usually characterized by their broad and flat shapes. Mauna Loa in Hawaii is a well-known example of a shield volcano.
Extrusive igneous rock.
The Krakatoa eruption in 1883 was a Plinian eruption, which is a highly explosive volcanic event characterized by the eruption of vast amounts of ash and volcanic material into the atmosphere. The eruption of Krakatoa was one of the most powerful volcanic explosions in recorded history.
they are on oceanic lithosphere.
shield
As of 2010, Popocatepetl is erupting. According to the Smithsonian National Museum of Natural History, continuous activity since Jan. 2005 has resulted in phreatic explosions, which occur when molten lava contacts water. In Popocatepetl's case the water inside the crater comes from the heat of the rising magma melting the glaciers on its peak.