pores
The SYNAPSE is the very small space between two neurons and is an important site where communication between neurons occurs.
rocks are formed from grains and grains are small and the rocks are big. Sedimentary rocks are formed when grains or sediments are compacted together.
when water is absorbed by rocks, and freezes, it will expand. therefore the rock will crack. Their bulk density increases (as the mass of the water contributes to the total mass of the rock) and the effective stress within the rock will decrease. This can ultimately cause the rock to fail without any increase in imposed loading.
An accessory mineral is a mineral present in small amounts in a rock, but not considered to be characteristic of the rock.
Because sandstone has wider particles than shale and this let's the water through.
Sandstone, as its name implies, is composed of many small grains of sand loosely held together. You may be able to rub some off with your hand. The grains will be small and there will be spaces between the grains. Granite on the other hand is formed from the melt underground, and has crystallized there. The crystals will be larger - up to cm size - and firmly bound. [Except if the granite is badly weathered.]
Fine grains of rocks are referred to as "clasts." The word "clast" comes from the Greek word "klastos," meaning "broken."
yes basalt has small grains
No. Pumice does not have grains.
A phobia of small spaces is called claustrophobia.
The SYNAPSE is the very small space between two neurons and is an important site where communication between neurons occurs.
A mineral's density increases as its mass per unit volume increases. If a mineral has a small mass and large unit volume, its density is smaller. Whereas, if a mineral has a large mass and a small unit volume, its density is greater.
Large grains, and crystals
The rock is conglomerate. The other rock would be Breccia if its grains were not rounded.
of course! the space between atoms is always very small, but there is always spaces, even in solids
A mineral is any naturally-occuring solid with a defined chemistry and crystalline structure. A crystal is the physical representation of a mineral which is large enough to see, either with the naked eye or hand lens. When minerals are small and need to be seen with a microscope most people start calling them "grains" (ex: a quartz grain in thin-section), but this is not an absolute.
A macro mineral is needed in large quantities whereas trace elements are minerals required in small quantities