it formes SEDIMENTry rock
Igneous and metamorphic rocks can be weathered and eroded by physical and chemical processes, breaking them down into smaller particles. These particles are then transported by wind, water, or ice and deposited in layers, forming sedimentary rocks through processes like compaction and cementation.
An igneous rock, just like any other rock, can be changed through metamorphic, igneous, and/or sedimentary processes. When exposed to high temp. and pressure, igneous becomes metamorphic. When re-melted, it becomes igneous again. When weathered/eroded, it becomes sedimentary.
Not every rock goes through the entire rock cycle in a linear progression from igneous to sedimentary to metamorphic and back to igneous. The rock cycle is more complex, with rocks undergoing various processes depending on environmental conditions. For instance, an igneous rock may weather and erode into sediment, forming sedimentary rock, but it doesn't necessarily have to transform into metamorphic rock. Additionally, rocks can be recycled in different ways, such as sedimentary rocks melting into magma or metamorphic rocks being directly uplifted and eroded.
Erosion, transportation of the eroded material, deposition of this material then lithification.
Erosion transports sediments from the original source through processes like wind, water, or ice. As the sediments are eroded, they are carried away and eventually deposited in a new location, forming sedimentary deposits.
When lava is eroded, it is broken down and transported and will eventually be buried and lithified, forming a sedimentary rock.
Yes, igneous rocks can be metamorphosed or weathered and eroded.
It gets eroded (broken down), then buried (maybe at the bottom of the sea), then the fragments become cemented as dissolved minerals fall out of solution to fill the cracks, forming a solid rock. The new rock is sedimentary (from sediment).
Yes, they can be eroded chemically and mechanically.
When an igneous rock is weathered and eroded into sediments by processes like wind, water, or ice, it can then be transported and deposited in layers. Over time, the sediments can undergo compaction and cementation, forming a sedimentary rock.
Igneous Rock
Igneous rocks form from the cooling and solidification of magma or lava. These rocks can then be weathered, eroded, and transported by natural processes like wind and water. Eventually, they may be buried, metamorphosed, and melted again to form new igneous rocks in a continuous cycle called the rock cycle.
Igneous rock can be found on the surface in areas of current or recent volcanism or in uplifted and eroded areas of past platonic intrusions, deep underground nearly anywhere, or in areas of past or present glaciations, where igneous rock has been eroded and deposited.
Eroded soil washes away and winds up in rivers, and eventually in lakes or oceans where is becomes sediment at the bottom. Rocks can be eroded into sand. Generally, they remain part of the soil, until the soil is eroded.
Magma cools into igneous rock. The igneous rock is uplifted to the surface and weathered by freeze/thaw cycles, acidic rainfall and plant root growth into smaller particles which are eroded and eventually settle as sand on the ocean floor. As more and more sand accumulates, the sand particles can lithify into sandstone, a sedimentary rock. With increasing depth, or from proximity to a heat source, the sandstone particles can recrystallize, forming the metamorphic rock quartzite.
Igneous rock, when exposed, will weather into smaller particles by mechanical and chemical means. Eventually the particles will be eroded and be transported by wind, water, ice, and gravity and eventually be deposited along with other sediments in a low lying area; could be the bottom of a sea, ocean or lake. As further and further sedimentation and accretion occur, the weight of overlying sediments compacts the particles, squeezing out air and water. Minerals then can bridge the gaps between particles, cementing them together into sedimentary rock.
Igneous and metamorphic rocks can be weathered and eroded by physical and chemical processes, breaking them down into smaller particles. These particles are then transported by wind, water, or ice and deposited in layers, forming sedimentary rocks through processes like compaction and cementation.