Shale started as mud. Mud is deposited in the bottom of lakes and seas.
Slate and shale are two rocks that can be separated into flat pieces.
Sedimentary rock is typically deposited in a geosyncline due to the accumulation of sediment over time. This process can result in the formation of various sedimentary rocks such as sandstone, shale, and limestone.
Sedimentary rocks made from fragments of rocks, minerals, and shells are known as clastic sedimentary rocks. Examples include sandstone, shale, and conglomerate. These rocks form when pre-existing rocks are weathered, eroded, transported, and deposited in layers.
Clastic sedimentary rocks are composed of particles ranging in size from clay (<0.004 mm) to boulders (>256 mm). These particles are derived from the weathering and erosion of pre-existing rocks, transported, and deposited to form clastic sedimentary rocks through processes like lithification.
No, shale rocks are not typically attracted to a magnet because they are composed primarily of clay minerals and other non-magnetic materials. Magnetism is generally not a characteristic of shale rocks.
Sedimentary rocks such as shale, sandstone, and limestone can be the source of deposited sediments through the process of weathering and erosion. These rocks are broken down into smaller pieces that are transported and eventually deposited to form new sedimentary layers.
Slate and shale are two rocks that can be separated into flat pieces.
Detrital rocks are sedimentary rocks that are composed of particles of weathered and eroded igneous, metamorphic, or other sedimentary rocks that have been deposited, compacted, and cemented together. Sandstone, conglomerate, shale, and breccia are examples of detrital sedimentary rocks.
Clastic sedimentary rocks form from the breakdown of larger rocks through weathering and erosion. The resulting sediments are deposited and undergo compaction and cementation to form rocks like sandstone, shale, and conglomerate.
Sedimentary rock is typically deposited in a geosyncline due to the accumulation of sediment over time. This process can result in the formation of various sedimentary rocks such as sandstone, shale, and limestone.
Sedimentary rocks made from fragments of rocks, minerals, and shells are known as clastic sedimentary rocks. Examples include sandstone, shale, and conglomerate. These rocks form when pre-existing rocks are weathered, eroded, transported, and deposited in layers.
sediment
Shale beaches are formed from the deposition of sediment form nearby shale cliffs which are eroded. The shale can also be deposited at a beach due to longshore drift.
Rocks formed from sediments deposited over time are called sedimentary rocks. These rocks are formed through the compaction and cementation of sediments, such as sand, silt, and clay, which have accumulated and solidified over millions of years. Examples of sedimentary rocks include sandstone, shale, and limestone.
Rocks with grains arranged in parallel layers are called sedimentary rocks. These rocks form when sediment such as sand, mud, or organic material is deposited and compacted over time. Examples include sandstone and shale.
Shale rocks turn into clay. The pressure make shale into clay.
Clastic sedimentary rocks are composed of particles ranging in size from clay (<0.004 mm) to boulders (>256 mm). These particles are derived from the weathering and erosion of pre-existing rocks, transported, and deposited to form clastic sedimentary rocks through processes like lithification.