No. A lahar is a mudflow formed by extrusive igneous material.
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The given options are not all intrusive igneous bodies. A batholith is an intrusive igneous body formed deep within the Earth's crust, while pyroclastic flows, lava flows, and lahars are volcanic hazards associated with volcanic eruptions.
No. A lahar is a mudflow formed from volcanic ash, which is extrusive. Because the material is transported by water, a lahar deposit is considered a sedimentary feature.
Lava is extrusive although rocks with the same chemical composition such as a dolerite are intrusive.
No. A lahar is a volcanic mudflow. Because lahars involve transport with water lithified lahar deposits are considered sedimentary.
Batholiths are an example of intrusive igneous formations, but lahars are not. Lahars are a result of extrusive ignenous activity. In other words, they are produced by volcanoes,
No. A pyroclast is an extrusive mass of rock or lava ejected by an explosive eruption.
An intrusive igneous rock.
A batholith is an example of an intrusive igneous body. Batholiths are large formations of intrusive igneous rocks that form beneath the Earth's surface through the slow cooling and solidification of magma.
A batholith is not necessarily in a volcano, but it is definitely involved with them. When a large body of magma cools inside the Earth's crust, creating a bed of volcanic rock, this is called a batholith. This can be a magma chamber or otherwise.
Intrusive igneous bodies that cut across existing sedimentary beds are said to be discordant. An example of a discordant intrusion is a batholith.
A mass of rock formed when a large body of magma cools inside the Earth is called an intrusion or pluton. These formations are referred to as intrusive igneous rocks and can vary in size and shape depending on the depth and cooling rate of the magma within the Earth's crust.