kimberliidimagma
Kimberliidimagma refers to the molten rock material from which kimberlite, a specific type of volcanic pipe rock, originates. Kimberlite is an ultramafic volcanic rock, typically found in the Earth's mantle, and is known for its association with diamonds. The magma that forms kimberlite is thought to originate at depths of 150 to 300 kilometers (93 to 186 miles) below the surface, a region known as the lithospheric mantle. This deep origin is a key characteristic that distinguishes kimberlite magma from magmas that form more common volcanic rocks.
The ascent of kimberliidimagma to the surface is rapid, often occurring as a violent explosive eruption. This