Volcanic bombs.
Large falling chunks of lava are known as "lava blocks" or "lava bombs." These are solid fragments ejected during volcanic eruptions, typically formed when volcanic gases expand and fracture the lava as it is expelled from a vent. Lava bombs can vary in size and shape, ranging from small pebbles to large boulders, and can cause significant damage upon impact due to their high temperature and kinetic energy. Their formation is common in explosive volcanic eruptions, where the force of the eruption propels the lava into the air.
a plateau
Pahoehoe and a'a refer to different texutres of lava flows. Although cindercones can produce lava flows, their main mode of eruption is called "fire fountaining" which tends to produce chunks of lava called scoria, rather than pahoehoe or a'a.
Cinder cones produce ash and chunks of lava rock called scoria.
composite
Large falling chunks of lava are known as "lava blocks" or "lava bombs." These are solid fragments ejected during volcanic eruptions, typically formed when volcanic gases expand and fracture the lava as it is expelled from a vent. Lava bombs can vary in size and shape, ranging from small pebbles to large boulders, and can cause significant damage upon impact due to their high temperature and kinetic energy. Their formation is common in explosive volcanic eruptions, where the force of the eruption propels the lava into the air.
nothing its just called lava fora reason.
They are called lava bombs they are chunks of semi molten rock thrown up from the volcano and then falling from a great height. When they hit the ground they have the shape of a bomb.
It is called aa
AA: jagged chunks of lava formed by rapid cooling on the surface of a lava flow
bombs
On poptropica in astro knights how do you jump on the rising lava without falling?
tupenu
a plateau
Any of the Lava Isles are where you can find obsidian chunks. There is no "best" place. Also, sometimes you can find them in the rock shops if another player has sold them recently.
Pahoehoe and a'a refer to different texutres of lava flows. Although cindercones can produce lava flows, their main mode of eruption is called "fire fountaining" which tends to produce chunks of lava called scoria, rather than pahoehoe or a'a.
The earth's crust is divided up into big chunks, and these chunks are essentially what we live on today. in between the chunks, where one meets another, there are lines running through the ground. These are called fault lines. Now, because the mantle is just molten lava, the crust just moves along as it pleases. When two chunks float around and rub up against one another, this causes vibrations on the fault lines. This also causes the ground to move and shake, what we call an earthquake :) Hope this helped