No, a dike is not a type of Lava flow.
A pluton is a dike.
blocky lava flow
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.
dike
Aa lava is the type of lava that forms a thick, brittle crust.
A pluton is a dike.
The seawall was built to act as a dike, protecting the town from flooding during storm surges.
blocky lava flow
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.
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.
dike
Aa lava is the type of lava that forms a thick, brittle crust.
Kilauea produces a'a and pahoehoe lava flows.
Pahoehoe is faster moving lava and AA is slower moving lava. Both types are found in basaltic type eruptions. They have different appearances. Pahoehoe is smooth and ropey where as AA is chunky and rough.(much like top of trees) Often a pahoehoe flow can change to an AA flow depending upon the type of slope it encounters. The steeper the slope the more likely AA lava will be present. Aa has more viscosity than Pahoehoe.
Pahoehoe lava.
it has pyroclastic flow and has small eruptions of ash.