How long is a cave?
The rates of cave development and surface lowering are very variable, depending on the limestone's own nature, the geology and hydrology of its setting, and the climate including any glacial phases.
As a rough guide a fair rate of rock-surface removal by a stream in a cave in Carboniferous Limestone in temperate latitudes, is a few millimetres / 1000 years.
A discrete cave passage can develop only while "active" (carrying its formative stream).
A humanly-enterable passage that is still active may be tens of thousands of years old as we can see it now; but its inception phase* as micro-conduits in the limestone's joints and other discontinuities carrying extremely slow flows of percolating ground-water, may well last hundreds of thousands of years.
Surface erosion of limestone uplands is different, as it depends on factors differing from those underground, but again, think of N X 105 or 6 years.
*Inception - a very recent hypothesis that gained Dr. David Lowe, a British caver and professional geologist, his PhD. Although still a 'hypothesis' his idea has attracted a lot of peer-interest and approval.
For most caves, in limestone, sufficient precipitation over sufficiently long time - but cave development also depends the region's geology and geomorphology.
millions of years
It doesn't necessarily matter what the minerals are, as long as they form from cooling magma or lava. Igneous rocks are formed by the solidification of cooled magma (molten rock). They may form with or without crystallization, either below the surface as intrusive (plutonic) rocks or on the surface as extrusive (volcanic) rocks.
surface waves, raleigh waves, and long waves.
Sea glass is made of any glass form that has been trashed and found its' way to the sea (most likely by dumping) only to be surf tumbled for a very long time until it has been changed in both texture and form by the natural movements of the ocean. The texture most often becomes like a sugar coated surface from the process of hydration. The change is form is when the edges are no longer sharp but smoothed and rounded.
it depends on the amount of rain received in the area because of soil erosion but it has known to be up to 100,000 years in the limestone caves in Naracoorte
It changes its cloak after a fight in a certain area. If you fight with it outside, or in long grass, then it takes on the Plant Cloak form. Beaches and caves will give Sandy Cloak, inside buildings will give Trash Cloak.
Caves usually form in areas with limestone or other soluble rocks that can be dissolved by water over long periods of time. Common locations for cave formation include regions with karst topography, such as in limestone landscapes or near volcanic activity, where lava tubes can create caves.
For most caves, in limestone, sufficient precipitation over sufficiently long time - but cave development also depends the region's geology and geomorphology.
Limestone caves are common because limestone is a soluble rock that dissolves easily in water. Over time, groundwater flowing through cracks in the limestone gradually enlarges these passages to form caves. Additionally, limestone is often found in areas with karst topography, characterized by sinkholes, underground rivers, and other features that promote the formation of caves.
That's extremely variable and specific to each cave, but you have to think in tens or hundreds of thousands of years.
Billions of years
Eels sleep in small caves under the water,at the bottem of the ocean and/or at the surface of the water.
Sea caves can take thousands to millions of years to form, depending on factors like the type of rock, wave action, and local geology. The process involves erosion from waves carrying abrasive materials that gradually wear away the rock to create a cave-like structure.
Energy, in the form of radiation, takes about 8 minutes to reach from the surface of Sun to the surface of Earth.
millions of years
The earliest they would have started to form would have been when their host limestone formation was upliftedand denuded so that karst processes could begin.