They are all clastic sedimentary rocks.
Shale, Sandstone, Conglomerate, Limestone, Breccia, Siltstone
Conglomerate, limestone, sandstone, and shale.
Some types of sedimentary rocks include limestone, sandstone, shale, and conglomerate. Sedimentary rocks form through the accumulation and lithification of sediment such as minerals, organic materials, and rock fragments that are transported and deposited by water, wind, or ice. The characteristics and composition of sedimentary rocks can provide valuable information about Earth's history and processes.
The three most common clastic sedimentary rocks are sandstone, shale, and conglomerate. Sandstone is composed of grains of sand cemented together. Shale is made of very fine particles like clay and mud. Conglomerate is a mix of larger rock fragments that are cemented together.
Some examples of clastic sedimentary rocks include sandstone, conglomerate, shale, and breccia. These rocks are formed from the accumulation of fragments of pre-existing rocks and minerals, which are then compacted and cemented together over time.
shale, siltstone, sandstone, and breccia are some.
Shale, Sandstone, Conglomerate, Limestone, Breccia, Siltstone
Conglomerate, limestone, sandstone, and shale.
Sandstone, conglomerate, and breccia are examples of clastic sedimentary rock, composed of particles of other rocks.
Compaction would likely be more significant as a lithification process for shale and sandstone due to their fine-grained composition, which is conducive to compaction. Conglomerate and breccia are coarser and have less room for compaction due to their larger grain sizes and irregular packing.
Sandstone: formed by the cementation of sand grains. Conglomerate: formed by the cementation of rounded pebbles. Siltstone: formed by the compaction of silt-sized particles. Shale: formed by the compaction of clay and silt particles.
Some types of sedimentary rocks include limestone, sandstone, shale, and conglomerate. Sedimentary rocks form through the accumulation and lithification of sediment such as minerals, organic materials, and rock fragments that are transported and deposited by water, wind, or ice. The characteristics and composition of sedimentary rocks can provide valuable information about Earth's history and processes.
Rocks that are categorized as sedimentary rocks include sandstone, breccia shale, limestone and selenite. Sedimentary rocks are classified by their grain size.
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.
The three most common clastic sedimentary rocks are sandstone, shale, and conglomerate. Sandstone is composed of grains of sand cemented together. Shale is made of very fine particles like clay and mud. Conglomerate is a mix of larger rock fragments that are cemented together.
shale
Shale forms in layers of sandstone or lime.