cinders
Acid lava cones are smaller and much steeper than ash/cinder cones. Acid lava cones are almost convex in shape and are formed due to thick lava that does not flow freely and cools before reaching very far. This gives in the conical 'dumpy' shape. While ash and cinder cones are more symmetrical and concave in shape. They are formed due to volcanic lava or volcanic bombs (of solidified lava) that was shot up in the air, cool and hardened and broke up into tiny pieces (of ash or cinders) before coming back down to the earth's surface.
five bombs
Syria's government use the cluster bombs to annihilate the Syrian citizens
mostly ordinary physics equations
As with pretty much any bomb or missile, a weapon's overall length and diameter essentially it comes down to the delivery vehicle. In the case of the early gravity bombs, anything over 5' in diameter wouldn't fit inside the bombers of that time period.
VOLCANIC ASH, VOLCANIC CINDERS, VOLCANIC BLOCKS & VOLCANIC BOMBS.
They differ in size and origin. Volcanic ash consists of fine material ejected by a volcano up to 2 mm (0.08 in) in diameter. Lapilli consists of larger material, ranging from 2mm to 64 mm (2.52 in) in diameter. Blocks and bombs are larger than 64 mm. Volcanic bombs form when molten lava is ejected during an eruption and solidifies in the air. A volcanic block is from material that is already solid when it is ejected, coming either from country rock or rock formed by previous eruptions.
The 4 different types of solid pyroclastics are volcanic bombs, lapilli, volcanic ash, and volcanic blocks
During a volcanic eruption, lava, tephra (ash, lapilli, volcanic bombs and blocks), and various gases are expelled from a volcanic vent or fissure.
tephra, ash, cinders, bombs, blocks, etc. depending on size.
Volcanic bombs, large blobs of magma that harden in the air, lapilli, pebblelike bits of magma that harden before they hit the ground, volcanic ash, forms when the gases in stiff magma expands, and volcanic blocks, large angular pieces of solid rock.
magma i think... :/
a pyroclastic flow is a cloud of volcanic bombs, volcanic blocks, volcanic ash, and lapilli. these flows can achieve speeds at over 125 miles per hour and can be more than 750 degrees Celsius.
Volcanic ash, cinders, and bombs are called tephra.
A volcanic mountain made up of volcanic ash, cinders, and bombs is called a Cinder Cone Volcano.
A volcanic mountain made up of volcanic ash, cinders, and bombs is called a Cinder Cone Volcano.
A volcanic mountain made up of volcanic ash, cinders, and bombs is called a Cinder Cone Volcano.