1. Volcanic Tuff and Volcanic Bomb
Sr.No. |
Volcanic Tuff |
Volcanic Bomb |
1 |
Volcanic Tuff is a type of igneous rock,formed during an explosive volcanic eruption. |
Volcanic bomb is a pyroclast which was semi-molten (viscous) while ejected from a volcanic vent and is therefore shaped while in flight. |
2 |
Tuff consist of volcanic ash with fragments less than 64mm. |
A mass of molten rock (tephra) larger than 64 mm (2.5 inches) in diameter. |
3 |
They reach the ground in extremely hot nature and then cool down gradually and form a stiff rock like structure. |
They cool into solid fragments before they reach the ground. Because volcanic bombs cool after they leave the volcano, they are extrusive igneous rocks. |
2. Central eruption and fissure type eruption
Sr.No. |
Central Eruption |
Fissure Type Eruption |
1 |
This type of eruption usually involves a single vent |
A fissure type has a lot of openings or vent unlike central type. |
2 |
The solid and molten rock materials ejected accumulate around. |
Lava,Flowing out of fissures,spreads out over extensive areas forming Lava sheets |
3 |
The vent forming a hill or a mountain is more or less conical in shape at the apex of these volcanic cones are funnel shaped depressions called craters |
This type of eruption involves a series of winds present along a fault line in the earths crust discharging enormous quantity of lava leading to the formation of lava planes and plateaus usually hundreds of square kilometers' in area. |
See Below Figure For Central And Fissure Type Volcanos