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no texture
Limestone grains are interlocking. The simple test to see if a rock's grains are interlocking is to put a drop of water on the surface. If the rock is interlocking, the water will remain on the surface. If it is not interlocking, the water will start to percolate through the rock. :).
schist
This will form a clastic sedimentary rock. If it is predominantly composed of sand sized grains then it will form a Sandstone.
The powder indicates the true color of the mineral and is an aid in mineral identification. That can also be called a streak.
no texture
i dont know, try another site.
Limestone grains are interlocking. The simple test to see if a rock's grains are interlocking is to put a drop of water on the surface. If the rock is interlocking, the water will remain on the surface. If it is not interlocking, the water will start to percolate through the rock. :).
no texture
Obsidian cools so quickly the mineral grains do not have time to form.
schist
yes
yes
Non-interlocking rock texture is a characteristic of clastic sedimentary rock, where particles of sediments have been cemented together by precipitated minerals. The particles may be loosely cemented, with spaces between particles. Rocks of this type tend to be 'soft' in that they are broken easily. An interlocking crystalline rock structure is formed by the progression of crystallization temperatures of various minerals as they form from solidifying magma. The solidification temperatures of the mineral constituents vary, and the last to crystallize is usually quartz, which infills any voids that remain. The resultant mineral structure is compact, hard, and resistant to weathering.
Quartz
This will form a clastic sedimentary rock. If it is predominantly composed of sand sized grains then it will form a Sandstone.
d. on the surface of the Earth