ROCKS (large structure)
↓(weathering)
SANDS (fine structure, relatively uniform particle sizes, cohesionless)
↓(further decomposing)
SOILS (usually very fine structure, uniformed or mixed particle sizes, usually cohesive, sometimes with organic matters)
ROCKS are classified into 3 types: IGNEOUS ROCKS, SEDIMENTARY ROCKS and METAMORPHIC ROCKS.
Rocks are considered as major component of earth surface and have a large continuous structure. Small isolated rocks are considered as STONES.
Something in between stones and sands are COBBLES and GRAVEL.
Rocks will, upon weathering, decompose into finer particles into SANDS and SOILS.
Sands are of particle size of range from 2~0.06 mm, the particles sizes of the same type of relatively uniform and sands are usually classified according to the particle size: COARSE SAND, MEDIUM SAND and FINE SAND. Sands are cohesionless.
The classification of soil is much more complicate because soils are composed of a large variety of particles of different size and , sometimes, organic matters ( peat soil). Usually, it is considered as soil if the major particle size is less than 0.06mm and hence cohesive in nature.
In fact, sands are only classified as a special type of soil ( under the type COHESIONLESS SOIL).
圖片參考:
http://i175.photobucket.com/albums/w130/bjoechan2003/My%20Cat%2020070128/DSCN0077.jpg?t=1169955111