Hematite.
The get compacted with burial and dewater. The grains from which they are made become cemented together and the sediments become sedimentary rocks.
Mineral water, rain water's acidity has drastically increased over the past couple of decades and is less pure than it used to be.
Enamel is over 95 per cent mineral. The principle mineral is hydroxyapatite which is a naturally occurring form of calcium phosphate. The remaning 5% is organic consisting of proteins called enamelins, amelogenins and albumin.
Color is what you observe when you look at a mineral. Streak is the color of the mineral when in a fine powder form. This can be observed by drawing a sample of the mineral over an unglazed porcelain tile and noting the color of the line left on the tile.
Rub a finger over the mineral
This is a chemical reaction between the acid and the mineral.
Fossils form through the process of mineral replacement beginning when an organism dies and is buried. Groundwater seeps around the organism, and the minerals in the water gradually replace the minerals in the hard parts of the organism. Over time these minerals turn into a stone replica of an organism.
Enamel is over 95 per cent mineral. The principle mineral is hydroxyapatite which is a naturally occurring form of calcium phosphate. The remaning 5% is organic consisting of proteins called enamelins, amelogenins and albumin.
Gross: total nitrogen transformed form organic to mineral form in soil over a period of time Net = Gross - the ammount re-taken up by microbes during the same period of time Net is a measure of "plant available" mineral nitrogen production.
Usually the mineral deposits a certain color or colors that you wouldn't see otherwise.
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There is no principal that states WHERE this may happen. The conditions that allow this to happen can form at different places over geologic time.