Gravel is a loose aggregation of rock fragments. Gravel occurs naturally on Earth as a result of sedimentary and erosive geological processes; it is also produced in large quantities commercially as crushed stone.
Gravel (largest fragment in this photo is about 40 mm (1.6 in))
Sand and gravel separator in a gravel pit in Germany
A gravel road in Finland
Naturally occurring sedimentary gravel bed
Crushed stone or angular rock is a form of construction aggregate, typically produced by mining a suitable rock deposit and breaking the removed rock down to the desired size using crushers. It is distinct from naturally occurring gravel, which is produced by natural processes of weathering and erosion and typically has a more rounded shape.
20 mm (0.79 in) crushed stone, used for construction aggregate and landscape applications
Crushed limestone quarry near Bellefonte, Pennsylvania
A crushed stone barge in China
Crushed stone laid as a road base