Obsidian is a natural volcanic glass with potentially sharp fracture edges.
Abrasion
breccia
Weathering attacks the surface of the rock most rapidly.
A sickle is a tool use to cut grass or grain. Flint bladed means that it uses sharp chips of flint rock for the cutting edges.
Obsidian is an extrusive rock that is a naturally occurring volcanic glass. It occurs when lava extrudes from a quickly cooling volcano, causing little crystal growth.
Abrasion
breccia
The definition of a shard is a piece of broken ceramic, metal, glass, or rock, typically having sharp edges. So with that definition, I would say that a shard of wood just means a piece of broken wood having sharp edges. If you are referring to the crossword puzzle hint, the answer is splinter.
The force of the water will have worn it smooth, with no sharp edges.
Pumice is so fine grained, it actually doesn't have a grain--because it is a natural volcanic glass. The rough texture is caused by the vesicular nature of the rock--trapped pockets of gas bubbles with sharp glassy edges.
Weathering attacks the surface of the rock most rapidly.
Sharp edges are knocked off by the tumbling effect created by moving water, much as a mechanical rock polisher does via a rotating drum. As more and more sharp edges are rounded, and as the rock is abraded by much smaller rock particles being transported by running water, the effect is a rounded smoothed rock surface.
A black rock full of energy is most likely obsidian, which is a natural volcanic glass formed during rapid cooling of lava. Obsidian is known for its sharp edges and ability to hold energy from the Earth.
Yes, slithers of which, when broken from a bigger lump (known as 'knapping') have sharp cutting edges.
A sedimentary rock called "breccia". The sharp angular pebbles making up the breccia could be igneous, sedimentary, or metamorphic. Breccias generally form close to the point of origin of the clast rock, having less time to round those sharp angular edges.
A sedimentary rock called "breccia". The sharp angular pebbles making up the breccia could be igneous, sedimentary, or metamorphic. Breccias generally form close to the point of origin of the clast rock, having less time to round those sharp angular edges.
Over time, the energetic stream will erode the sharp edges and corners of the cubic rock, gradually smoothing out its surface and rounding its edges. The rock will likely become more rounded and smoother as it is continuously bombarded by the swift-moving water.