From your statement it sounds like you are referring to an igneous dyke rather than a sill, however see the following:
A sill is a sheet of intruded magma that forms between to layers of older "country" rock. This is technically described as a "concordant sheet intrusion". If it is later over turned due to tectonic folding it may be vertical but as it was originally emplaced between and parallel to pre-existing rock layers, it is still an igneous sill! However if the intrusion cross cuts the bedding planes of the country rock - known as a discordant intrusion (and was originally (sub)vertical at the time of emplacement) it is known as a dyke.
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Yes, that's correct. Sills are igneous rock formations that form when magma is intruded horizontally between rock layers and then solidifies underground. If the magma solidifies vertically underneath the surface, it will create a sill structure.
Granite and basalt are made when magma cools. Granite forms from slow-cooling magma underneath the Earth's surface, while basalt forms from rapidly-cooling magma on the surface.
Beneath volcanic features at Earth's surface lies a magma chamber filled with molten rock. As magma rises towards the surface, it can accumulate in reservoirs below the volcano, creating the potential for eruptions. This molten rock comes from the Earth's mantle through volcanic pipes and conduits.
Magma is liquid rock before it reaches the surface magma which reaches the surface is called lava.
it's called lava! lava is what's on the surface of a volcano, and magma is what's underneath
Yes, that's correct. Sills are igneous rock formations that form when magma is intruded horizontally between rock layers and then solidifies underground. If the magma solidifies vertically underneath the surface, it will create a sill structure.
The rock that melts underneath the Earth is called magma. Magma is formed from the melting of the Earth's mantle and can rise to the surface to form igneous rocks when it solidifies.
Granite and basalt are made when magma cools. Granite forms from slow-cooling magma underneath the Earth's surface, while basalt forms from rapidly-cooling magma on the surface.
it's called lava! lava is what's on the surface of a volcano, and magma is what's underneath
Beneath volcanic features at Earth's surface lies a magma chamber filled with molten rock. As magma rises towards the surface, it can accumulate in reservoirs below the volcano, creating the potential for eruptions. This molten rock comes from the Earth's mantle through volcanic pipes and conduits.
Magma is liquid rock before it reaches the surface magma which reaches the surface is called lava.
When magma cools at the surface of the Earth, it cools very quickly and hardens on the Earths crust. However, it continues flowing underneath, forming interesting textures.
The igneous rock could have been erupted as lava on the surface, or intruded into the sedimentary rock layers as magma underneath the surface (a sill).
Magma is lava underneath the earth. The tectonic plates of the earth float on it.
Yes, all volcanoes erupt because the magma underneath or in the volcano is under pressure, which forces the magma to the surface, where there is less pressure. However, volcanoes form in different places.
it's called lava! lava is what's on the surface of a volcano, and magma is what's underneath
magma