No, it is not a rock, it is a mineral/crystal.Amazonite is a green variety of microcline feldspar, which does occur in some intrusive, granitic Igneous rocks.
microcline is the answer
They are all found in Granite
It is usually potassium feldspar, either microcline or orthoclase.
An amazonite is a gem variety of microcline feldspar, varying from bright verdigris to bluish-green.
1.The green variety of microcline amazonite is used as an ornamental lapidary material.2.Microcline is used mainly in the manufacture of porcelain. It is ground very fine and mixed with kaolin and quartz. Upon heating, the feldspar fuses and acts as a cement binding the materials together. Fused feldspar also is the main constituent in the glaze on porcelain.3.Sometimes microcline is also used to supply alumina in the manufacture of glass.by Maham kainat :P
1.The green variety of microcline amazonite is used as an ornamental lapidary material.2.Microcline is used mainly in the manufacture of porcelain. It is ground very fine and mixed with kaolin and quartz. Upon heating, the feldspar fuses and acts as a cement binding the materials together. Fused feldspar also is the main constituent in the glaze on porcelain.3.Sometimes microcline is also used to supply alumina in the manufacture of glass.by Maham kainat :P
An amazonstone is a blue-green variety of microcline feldspar used as a gemstone, found at Crystal Peak and Pike's Peak in Colorado.
granite
plagioclase, microcline, rhodonite, turquoise, wollastonite, amblygonite, and many more.
Alkali feldspar has the general formula (K,Na)AlSi3O8, but varies in crystal structure depending on the temperature it formed at. The formula actually is a blend ranging from all sodium (albite) to all potassium (microcline), but albite is also one endpoint in the plagioclase series so we classify albite there. This mineral is often called potassium feldspar or K-feldspar, because by definition potassium always exceeds sodium in its formula. It comes in three different crystal structures that depend on the temperature it formed at. Microcline is the stable form below about 400° C. Orthoclase is stable above 500° C and sanidine is stable above 900° C. In a plutonic rock that cooled very slowly to yield large mineral grains, it's safe to assume that this is microcline. In the field, workers generally just write down "K-spar" and leave it at that until they can get to the laboratory. Alkali feldspar is generally white, buff or reddish and is not transparent, nor does it show the striations of plagioclase. A green feldspar is always microcline, the variety called amazonite.
Granite contains plagioclase feldspar and potassium feldspar. It really depends on the composition of the magma from which it forms. If the granite has a lot of pink in it, chances are it is potassium feldspar (K-Spar). If it is dominated by white, then the feldspar is probably plag.