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.
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.
Volcanic ash is fine particles of fragmented volcanic rock that are ejected into the air during an eruption, while volcanic bombs are larger, often rounded pieces of molten rock that solidify before landing. Ash is carried by winds and can travel long distances, whereas volcanic bombs usually fall near the eruption site due to their larger size and weight.
The 4 different types of solid pyroclastics are volcanic bombs, lapilli, volcanic ash, and volcanic blocks
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.
tephra, ash, cinders, bombs, blocks, etc. depending on size.
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 ;)
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.
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.
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.
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.
A volcanic mountain made up of volcanic ash, cinders, and bombs is called a Cinder Cone Volcano.