cinders
five bombs
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.
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.
lapilli. Lapilli are small fragments of magma expelled during a volcanic eruption that solidify before hitting the ground. They are larger than volcanic ash but smaller than volcanic bombs.
Fragmental volcanic material is often referred to as pyroclastic or tephra, which includes ash, lapilli, and larger volcanic blocks and bombs produced during explosive volcanic eruptions.
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
tephra, ash, cinders, bombs, blocks, etc. depending on size.
The larger-sized tephra is known as volcanic bombs. These are ejected as incandescent lava fragments that solidify while flying through the air and can reach several meters in diameter. Volcanic bombs are usually formed during explosive eruptions at volcanoes.
Lapilli--Lapilli is pyroclastics the size of walnuts.Cinders-- Cinders are a type of pyroclastic material the size of a pea. According to the text, Earth An Introduction to Physical Geology, Cinders come in different forms when "ejected lava blobs are pulverized by the escaping gases".Blocks-- Blocks are particles larger than Lapilli's and are formed by harden lava.Bombs-- Bombs too help to produce blocks, but they are ejected as lava. They take on an streamline shape. They usually tend to fall on the slopes of a cone volcano and they can be ejected far from the volcano due to the force of escaping gasesI answered this earlier but this is a better answer ;)
Tephra consists of volcanic ash, cinders, and volcanic bombs. Tephra is ejected during explosive volcanic eruptions and can vary in size from tiny ash particles to large volcanic bombs.
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.
The various types of material ejected by a volcano are called volcanic products, which can include ash, lava flows, pyroclastic flows, volcanic gases, and volcanic bombs. These materials vary in size, composition, and behavior depending on the type of volcano and the eruption style.
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.