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Once emplaced in this comparatively shallow and cold environment, the magma solidifies by crystallization and further gas release (second boiling).
The huge allochthonous deposits emplaced in this region (the so-called "Olistostrome" of the Gulf of Cadiz) are described in terms of three different domains on the basis of the seismic architecture, the main tectonic features and the nature of the basement, oceanic or continental.
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Geologic studies have shown that The Volcano and its eruptive products were emplaced in the past 400 years; this is well after the last glacial period, which ended about 10,000 years ago.
These domains are inferred to represent dismembered Ferrar intrusions emplaced in the source area of the debris avalanche; shallow emplacement of Ferrar magmas caused a slope failure that mobilized the uppermost Beacon Supergroup, and the silicic ash deposits, into a pre-existing valley or basin.
Allochthonous (transported) continental blocks thus were emplaced in the Cordillera Oriental of Ecuador, Colombia, and Venezuela at the end of the Silurian Period (about 419 million years ago).
About 2 billion years ago the Bushveld Complex which is one of the largest differentiated igneous bodies on Earth, containing major deposits of platinum, chromium, and vanadium was emplaced in the northern Kaapvaal craton.
Igneous rocks are subdivided into two categories: intrusive (emplaced in the crust), and extrusive (extruded onto the surface of the land or ocean bottom), in which case the cooling molten material is called lava.
There were intermittent vulcanian explosions for three months after the lava was emplaced in the crater.
The lava emplaced in the crater was too flat to be defined as a lava dome, but was too solid to be called a lava lake.
Given that the quantity of soil added periodically is marginal and discounting for recycling and decomposition, only about 60%% of these may be emplaced in the landfill.
The thickest sills are up to 200 m thick, representing extensive (>200 km) sheets emplaced in the organic-rich shales of the lower Ecca Group.
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