The most famous spot for lava tubes on Earth is Hawai'i. Because of the geography, the Lava Tubes on Big Island are the biggest in the World. Kazumura Cave is 61.407 m long and has a height difference of 1102 m from end to end.
Basaltic, low viscosity lava would form lava tube caves.
The solidified lava forming the walls of the lava tube will act to insulate the molten lava. It will therefore cool more slowly than lava at the surface and so will have a lower viscosity (it will be more runny) and so will flow faster than lava at the surface.
The tunnel is called a lava tube or magma tube.It's called a conduit.conduita tube or vent tube
Lava tubs form as a result of pahoehoe lava flows. As one of these flows progresses, it builds of a layer of rock on top of it. eventually, thus becomes thick enough to support is own weight, and forms an insulating tube through which lava can flow.
It travels through a "Pipe" and explodes out the "Vent", or possibly the "Side Vent", and another world for the hole at the top is the Crater.
Basaltic, low viscosity lava would form lava tube caves.
The most famous spot for lava tubes on Earth is Hawai'i. Because of the geography, the Lava Tubes on Big Island are the biggest in the World. Kazumura Cave is 61.407 m long and has a height difference of 1102 m from end to end.
Lava tube caves form when low viscosity lava flows beneath the hardened surface of lava flow while the volcano is active. Then when the volcano is dormant or extinct, it leaves cave like channels.
"Basic", or low-silica, basalt lava, as its viscosity is relatively low.
Land caves can be found all around the world, with significant locations including the United States, Mexico, Australia, China, France, and Spain. They are typically formed in areas with limestone, volcanic rock, or gypsum deposits that have been eroded by natural processes like water, wind, and tectonic activity.
Yes. Ape Cave - two mile long lava tube, Gardner Cave - 1000' long limestone cave Ice Cave - 400' long lava tube Source: http://www.goodearthgraphics.com/showcave/wa.html
They both depend on eruptions for their formation but lava tubes form only in large flows of low-viscosity, basaltic,lava. I don't know if this applies to Mt. Pinatubo.
Most caves are in limestone or dolomite rocks. Some (e.g. Carlsbad Caverns) are in gypsum rocks. But caves can also exist in lava deposits (e.g. lava tube caves), marble rocks (i.e. metamorphosed limestone), and many other types of rocks at lower rates, depending on various variables.
Not a pattern in a mathematical sense, no, but the vast majority of the world's caves are in limestone uplands of appropriate structural and hydrological characteristics for cave development. They are very rare in Chalk, for instance, even though Chalk is a type of Limestone. Limestone is a very common and widespread range of sedimentary calcium-carbonate rocks, so caves are found in very many countries. Another important but much rarer type of cave is the Lava Tube, but this can only form in flows of low-viscosity lava, retricting them to a few locations.
lava tube
They form in relatively low-viscosity "basic" (low-silica, basalt) lava flows by the surface solidifying over still-flowing molten rock. If the molten lava drains away it leaves a cavity within the mass of the flow. Main lava caves of the word are on Iceland and Hawaii. Fingal's Cave, on the Isle of Staffa, is in columnar flood-basalt but is a marine-erosion feature.
Most caves are the result of erosion. The vast majority by far are in limestone, as it is soluble in weakly-acid ground-water (chemcial weathering). Mass-movement fissures result from a type of landslip mechanism. Talus caves are cavities between boulders and the rock-fce from which they have fallen. Sea caves come from weathering and erosion by wave attack on cliffs. About the only exception is the Lava Tube, formed by still-molten, low-viscosity lava flowing out from below its solidified crust.