No, generally not. Most composite volcanoes erupt more viscous, high-silica material than what would form a'a. So block lava would be more common.
A'a can occur at composite volcanoes, but block lava flows, which are far more viscous, are more common.
Aa lava is a basaltic lava with a flow characterized by rough surfaces of clinker.
When volcano lava cools at the surface, it may form different features such as lava rock formations like basalt columns, lava tubes, and aa or pahoehoe lava flows. These features depend on the cooling rate and composition of the lava.
Thick, stiff lava that does not flow easily is known as aa lava. Aa lava has a rough, blocky texture due to its high viscosity, making it difficult for the lava to flow smoothly. Aa lava typically moves in a jerky, slow manner and can form sharp, jagged edges as it solidifies.
A'a lava forms rough jagged edges as it cools and solidifies. It is characterized by its blocky and sharp texture, which can make it difficult to walk on. A'a lava flows tend to move slower compared to pahoehoe lava flows.
Shield volcanoes have low viscosity basaltic lava, which typically creates pahoehoe and AA lava flows due to their ability to flow easily. Composite volcanoes have higher viscosity lava, such as andesitic or dacitic, which tend to form thicker and blockier lava flows rather than pahoehoe and AA flows.
A'a can occur at composite volcanoes, but block lava flows, which are far more viscous, are more common.
Usually neither. A'a and pahoehoe lavas are both of mafic composition (rich in iron and magnesium, poor in silica) and form basalt when they cool. Composite volcanoes usually erupt material of intermediate to felsic composition (felsic is rich in alkalis, aluminum, and silica), with lavas cooling into rocks such as andesite, dacite, and rhyolite.
Aa lava is a basaltic lava with a flow characterized by rough surfaces of clinker.
It is called aa
When volcano lava cools at the surface, it may form different features such as lava rock formations like basalt columns, lava tubes, and aa or pahoehoe lava flows. These features depend on the cooling rate and composition of the lava.
Thick, stiff lava that does not flow easily is known as aa lava. Aa lava has a rough, blocky texture due to its high viscosity, making it difficult for the lava to flow smoothly. Aa lava typically moves in a jerky, slow manner and can form sharp, jagged edges as it solidifies.
The difference between Pahoehoe lava and AA lava is that pahoehoe lava is smooth and AA lava is jagged.
A'a lava forms rough jagged edges as it cools and solidifies. It is characterized by its blocky and sharp texture, which can make it difficult to walk on. A'a lava flows tend to move slower compared to pahoehoe lava flows.
If a geologist finds AA rock, it is likely that the rock contains basaltic lava flows or volcanic material, as "AA" refers to a type of lava that has a rough, jagged surface. This texture forms when lava cools quickly and has a higher viscosity. AA lava is typically associated with shield volcanoes and can indicate past volcanic activity in the area.
Both blocky lava and aa lava are types of viscous, cooler lava flows that form rough, jagged surfaces. They are characterized by their slow movement and blocky appearance due to the solidifying of the lava flow before it fully cools.
A quiet eruption typically produces basaltic lava. This type of lava is low in viscosity and flows easily, resulting in gentle, slow-moving lava flows. It often forms shield volcanoes with broad and gently sloping sides.