@got2know12,
It a kind of quartzite with distinct layering. You can see the grains and the staining. Itd be nat f you could find the "ledge" from which it was flaked off.
Seeing the rock In place is far better than seeing it sitting on a table. Part pf geology that the professionals do is to determine where the rocks started, when, an how they were deposited, Because knowing allthat they can derive "conceptual models" and you can compare the rock to other sites (All this is often needed to do things like "prospecting" or seeking out gemstones.