because it falls into little ice and formes into rocks and turns solid.
Rocks can break into tiny pieces through weathering processes such as frost wedging, where water gets into cracks in rocks and expands when it freezes, causing the rock to break apart. Another way is through chemical weathering, where minerals in the rock react with water and air, causing the rock to crumble into smaller pieces.
Volcanoes can erupt various materials such as lava (molten rock), ash (tiny rock particles), gases (including water vapor, carbon dioxide, and sulfur dioxide), and sometimes rocks, boulders, and volcanic bombs (larger ejected rock fragments).
Weathering is the process that breaks down rocks into tiny pieces. This can happen through physical weathering (such as ice wedging or abrasion) or chemical weathering (like acid rain or oxidation). Over time, these processes can turn large rocks into smaller fragments, a key step in soil formation.
Clastic sedimentary rocks are formed from particles of pre-existing sedimentary, metamorphic, or igneous rock that are deposited, compacted, and cemented together by natural processes.Clastic sedimentary rock is made of fragments of rocks cemented together by a mineral such as calcite or quartz.
cinder-cone volcano
Large rocks break down into tiny rocks through the process of weathering and erosion. Weathering breaks down the rocks into smaller pieces through physical or chemical processes, while erosion transports these smaller rock fragments to new locations. Over time, repeated cycles of weathering and erosion can further break down large rocks into tiny rocks.
All rocks have cracks in them. If water fills the cracks and freezes, it expands and pushes the rock apart.
Rocks can break into tiny pieces through weathering processes such as frost wedging, where water gets into cracks in rocks and expands when it freezes, causing the rock to break apart. Another way is through chemical weathering, where minerals in the rock react with water and air, causing the rock to crumble into smaller pieces.
Tiny pieces of rock are called 'grains' or 'particles'. These small fragments of rock can vary in size from sand grains to silt or clay particles.
Volcanoes can erupt various materials such as lava (molten rock), ash (tiny rock particles), gases (including water vapor, carbon dioxide, and sulfur dioxide), and sometimes rocks, boulders, and volcanic bombs (larger ejected rock fragments).
Galena breaks into tiny cubes due to its crystal structure, which is cubic. When it fractures, it tends to break along its natural cleavage planes, resulting in the formation of small cube-shaped fragments.
Weathering breaks up the rock by rubbing parts of old rocks against it, this causes the rock to break up into tiny pieces and it rubs agaist other rocks. it continues on for a looong time... however it take a long time for it to break up the rock. hope it helps!!
Clastic sedimentary rocks. Clastic sedimentary rocks are formed when small sediment particles are compacted and cemented together. This happens when the sediments are glued together by tiny crystals or chemicals from fluids that have precipitated in the pores between the sediments.
Water expands when freezing.
Weathering is the process that breaks down rocks into tiny pieces. This can happen through physical weathering (such as ice wedging or abrasion) or chemical weathering (like acid rain or oxidation). Over time, these processes can turn large rocks into smaller fragments, a key step in soil formation.
Various forms of human activity break down rocks, from drilling and mining to creating acid rain, which dissolves rocks faster than less-acid rain. Acid rain is created when sulfur dioxide, nitrogen dioxide, and other industrial waste gases are released into the air. Ice breaks rocks when water enters tiny cracks, and then expands when it freezes, forcing the cracks apart.
Clastic sedimentary rocks are formed from particles of pre-existing sedimentary, metamorphic, or igneous rock that are deposited, compacted, and cemented together by natural processes.Clastic sedimentary rock is made of fragments of rocks cemented together by a mineral such as calcite or quartz.