The heaver rocks settle to the bottom and the lighter ones stay on the top and they form layers!
Sedimentary rocks form when layers of rock particles are compacted or cemented together over time. Examples of sedimentary rocks include sandstone, shale, and limestone.
Detrital sedimentary rocks are made from weathered rocks.
Sedimentary rock is most likely the result of compaction and cementation of particles. This process involves the gradual accumulation, burial, and lithification of sediment to form rock. Examples of sedimentary rocks include sandstone, shale, and limestone.
Detrital sedimentary rock. clastic sedimentary A+
If the original rock is eroded or broken away and then returned to sedimentary-forming conditions, it will form another sedimentary.
Sedimentary rocks form when layers of rock particles are compacted or cemented together over time. Examples of sedimentary rocks include sandstone, shale, and limestone.
The rock described would be a clastic sedimentary rock.
Sedimentary rock melts, then it cools to form Igneous rock. Hoped this helped. :)
Sandstone is the sedimentary rock formed from weathered rock.
Sedimentary rock
Detrital sedimentary rocks are made from weathered rocks.
Sedimentary rocks are formed when layers of rock particles carried by wind and water are compacted and cemented together. Sandstone, shale, and conglomerate are examples of sedimentary rocks formed through this process.
Sedimentary rock is most likely the result of compaction and cementation of particles. This process involves the gradual accumulation, burial, and lithification of sediment to form rock. Examples of sedimentary rocks include sandstone, shale, and limestone.
Detrital sedimentary rock. clastic sedimentary A+
Sandstone is one possible form.
yes sedimentary rock countain all particles from both igneous and metamorphic rock.
If by particles you mean the size of the crystals, then the crystals in metamorphic rock are often larger than in the sedimentary rock. High heat and pressure can cause the minerals to recrystallize. This would be the case in the metamorphosis of limestone (sedimentary) to marble (metamorphic).