Investigating the Rate of Lava Flows Down the Side of a Volcano

My purpose of investigating the flow velocity of lava to the volcano side is to investigate the factors affecting the speed of lava flowing to the volcano side and the flow velocity of the volcano. In this plan, there are various variables • Slope angle • Volcano surface • Lava amount • Lava temperature • Environmental condition • Lava viscosity • Flow distance • Ejection force I decided to investigate the angle slope as I will investigate in Scho

Imagine a volcanic eruption. Lava flows down from the volcano and destroys all of the way, but as it cools, new lands are formed. Initially, the new land will be barren and will not live in that area. But after a while, simple creatures will begin to colonize the new land. Creatures engaged in primary inheritance are called Pioneer species. Typical pioneer species include simple lichens, algae and fungi. These simple creatures begin to degrade the resources in the environment and make them suitable for later introduction into more complex species such as vascular plants. When these creatures carry out their living process, they produce waste and some die. This leads to the formation of soil organic matter

If the eruption is non-explosive like the typical eruption of Hawaii Volcano, lava flows will occur. Lava comes from the cracks on either side of the volcano, or through vents in the crack. Tephra rarely decays during a non-explosive eruption. Non-explosive volcanic eruptions are characterized by basaltic lava and the type of volcano it forms Shield volcanologists (scientists who are studying volcanoes) are often interested in deep processes of rocks deep inside volcanoes. By studying the chemical characteristics of specific minerals in volcanic rocks in detail, they can begin to master these processes. They can also start to understand what happens when the first magma is generated.