No, a dike is not a type of Lava flow.
A pluton is an igneous rock formation formed beneath the Earth's surface. A dike is a vertical or near-vertical geological formation where magma has intruded into pre-existing rock. A lahar is a type of volcanic mudflow made up of water, ash, and other debris flowing rapidly down the slopes of a volcano. A lava flow is the movement of molten rock on the Earth's surface during a volcanic eruption. Pyroclasts are rock fragments ejected during a volcanic eruption, such as ash, lapilli, and volcanic bombs.
A dike is an intrusive igneous rock. It is a vertical intrusion that is usually associated with a central magma chamber. It is intrusive because it usually does not reach the surface. When a dike does reach the surface, the magma it countains erupts and forms an extrusive lava flow.
Arenal Volcano in Costa Rica mainly produces basaltic andesite lava. This type of lava is characterized by its intermediate silica content, which results in a thick, slow-moving lava flow.
dike
Pahoehoe lava flows exhibit a fairly smooth, unfragmented, and ropy surface. This type of basaltic lava flow has a characteristic appearance due to its low viscosity, which allows it to flow and solidify in a smooth manner.
A dike is not a machine, it does not change the direction of any force or amplify any force, it is merely an obstacle to the flow of water.
A pluton is an igneous rock formation formed beneath the Earth's surface. A dike is a vertical or near-vertical geological formation where magma has intruded into pre-existing rock. A lahar is a type of volcanic mudflow made up of water, ash, and other debris flowing rapidly down the slopes of a volcano. A lava flow is the movement of molten rock on the Earth's surface during a volcanic eruption. Pyroclasts are rock fragments ejected during a volcanic eruption, such as ash, lapilli, and volcanic bombs.
The type of lava flow that Mt. Kilauea has is a pahoehoe flow. This flow involves lava flowing into sheets after eruption. Once its top has cooled, the bottom layer moves under it resembling "a rope."
A dike is an intrusive igneous rock. It is a vertical intrusion that is usually associated with a central magma chamber. It is intrusive because it usually does not reach the surface. When a dike does reach the surface, the magma it countains erupts and forms an extrusive lava flow.
Arenal Volcano in Costa Rica mainly produces basaltic andesite lava. This type of lava is characterized by its intermediate silica content, which results in a thick, slow-moving lava flow.
dike
The dike formed after lava flowed from the volcano.
Pahoehoe lava flows exhibit a fairly smooth, unfragmented, and ropy surface. This type of basaltic lava flow has a characteristic appearance due to its low viscosity, which allows it to flow and solidify in a smooth manner.
it has pyroclastic flow and has small eruptions of ash.
A'a Lava.
Aa
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...