Serving platter. Arrange the leaves of lettuce on your cute plate. Make an oval at the bottom with slices of cucumber (this is the turkeyâs body). Slice the peppers into half-circle rings, keeping the bottoms of the peppers for later. Arrange the pepper slices above the cucumbers â yellow, then green, then red ones.
Stalactites form when water containing dissolved calcium bicarbonate from the limestone rock drips from the ceiling of a cave. As the water comes into contact with the air, some of the calcium bicarbonate precipitates back into limestone to form a tiny ring, which gradually elongates to form a stalactite. Stalagmites grow upwards from the drips that fall to the floor. They spread outwards more, so they have a wider, flatter shape than stalactites, but they gain mass at roughly the same rate. Limestone stalactites form extremely slowly â usually less than 10cm every thousand years â and radiometric dating has shown that some are over 190,000 years old.
A stalactite also known as dripstone, is like a stone icicle on the ceiling of a limestone cave. It develops when water, in which minerals (usually primarily calcium carbonate) is dissolved, drips though cracks in cave ceiling. As the water falls, it leaves behind microscopic amounts of the mineral. Over time, this collects to form an icicle-like structure. Note that a stalagmite is like an upside-down stalactite growing up from the floor. When water drips from a stalactite and hits the cave floor, there is often a microscopic mineral deposit left there as well. This deposit builds up over time. It is possible, by the way, for a stalactite and stalagmite to meet, forming a mineral column.