The other way round. Eruptions caused the extinctions. Direct affect of the the lava and the increase in dust in the air causing cooling and the gas itself making the air poisonous
Underwater eruptions cause tsunamis and cause lava to form and underwater ridge.
run like crazy cause the lava is coming
Basaltic magmas are associated with fissure eruptions creating lava flows spilling out from cracks in the crust. This is because basaltic magmas are more viscous and contain a lower concentration of gases than rhyolitic magma and therefore are unable to build up sufficient pressure to produce explosive eruptions.
Different types of lava result in different types of volcanic eruptions. Basaltic lava, which is low in viscosity, typically leads to effusive eruptions characterized by gentle flows. Andesitic or dacitic lava, with higher viscosity, can cause explosive eruptions with pyroclastic flows and ash clouds. Rhyolitic lava, the most viscous type, tends to form dome eruptions with slow-moving lava flows and explosive activity.
Lava combs are considered destructive features because they are formed by volcanic eruptions that can cause widespread damage to the surrounding environment. They are often associated with explosive eruptions and the deposition of lava and other volcanic materials, which can lead to destruction of landscapes and ecosystems.
Yes, repeated eruptions of fluid lava from fissures can lead to the accumulation of thick layers of basaltic lava flows known as flood basalts. These eruptions commonly occur in large igneous provinces and can cover extensive areas, altering the landscape significantly.
Volcanic eruptions.
Lava can be explosive if it is high in gas content, such as dissolved water vapor or carbon dioxide, which can cause pressure to build up and lead to explosive eruptions. On the other hand, lava can be non-explosive if it is low in gas content and flows more easily without building up pressure, resulting in effusive eruptions with slower lava flows.
No, pahoehoe and aa lava are typically produced during non-explosive eruptions. Pahoehoe lava has a smooth, ropey texture, while aa lava is rough and jagged. Explosive eruptions typically produce ash, pyroclastic flows, and lava domes.
Mount Etna typically erupts with basaltic lava, which is low in viscosity and flows more easily compared to other types of lava. This can result in effusive eruptions with lava fountains and lava flows traveling long distances. The low viscosity of basaltic lava allows gases to escape more easily, reducing the risk of explosive eruptions.
kilauea
More lava comes out.