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These skeletons accumulate over time, forming deposits of diatomite. It is finely porous, is low in density, and has low thermal conductivity. These microscopic organisms construct intricate cell walls, called frustules, primarily composed of amorphous silica (hydrated silicon dioxide).

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It occurs in earthy beds that somewhat resemble chalk, but it is much lighter than chalk and will not effervesce in acid. Diatomaceous earth is a soft and friable rock. It is a very porous rock with a fine particle size and a low specific gravity.

The primary component of diatomite is silica (sio2), which may comprise up to 90% of its composition

Additionally, it contains other minerals such as iron oxides, aluminum oxides, and calcium carbonate in varying amounts. Diatomite is found under various soil layers in locations where seas or lakes once existed The high content of organic silicon and calcium in these fossilized diatoms gives diatomite its characteristic white color.