Strip mining is the most common method.
quartz and clay
Shale is a detrital rock, meaning it is composed of fragments of other rocks and minerals. It forms from the compaction and cementation of silt and clay particles. There are organic-rich shales as well, but they are still considered detrital in nature.
A fine-grained detrital rock that breaks into chunks or blocks is likely a shale. Shale is composed of clay minerals and silt-sized particles compacted together. It tends to break along bedding planes, forming flat chunks or blocks.
Clay minerals and quartz are the chief constituents of most sedimentary rocks in this category. To answer why, clay minerals are the most abundant product of the chemical weathering of silicate minerals, especially the feldspars. Clays are fine-grained minerals with sheetlike crystalline structures similar to the micas. Quartz is abundant because it is extremely durable and very resistant to chemical weathering. Thus, when igneous rocks such as granite are attacked by weathering processes, individual quartz grains are freed.
Detrital sedimentary are classified according to the size and shape of their sediments.
quartz and clay
Quartz and Clay.
Clay particles. Less than 2 micrometres in diameter.
The most common minerals found in detrital sedimentary rocks are quartz, feldspar, and clay minerals. These minerals are often derived from the erosion and weathering of igneous and metamorphic rocks.
Shale is a detrital rock, meaning it is composed of fragments of other rocks and minerals. It forms from the compaction and cementation of silt and clay particles. There are organic-rich shales as well, but they are still considered detrital in nature.
A detrital sedimentary rock made up of clay-sized particles that require no cementation to hold together is called shale. Shale forms from the compaction of clay minerals without the need for additional cementing materials.
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.
Clay, Silt, Sand, Granule, Pebble, Cobble and Boulder.
A fine-grained detrital rock that breaks into chunks or blocks is likely a shale. Shale is composed of clay minerals and silt-sized particles compacted together. It tends to break along bedding planes, forming flat chunks or blocks.
Clay minerals and quartz are the chief constituents of most sedimentary rocks in this category. To answer why, clay minerals are the most abundant product of the chemical weathering of silicate minerals, especially the feldspars. Clays are fine-grained minerals with sheetlike crystalline structures similar to the micas. Quartz is abundant because it is extremely durable and very resistant to chemical weathering. Thus, when igneous rocks such as granite are attacked by weathering processes, individual quartz grains are freed.
the shape and size of the sediments
Reasoning : soil particles the diameters of which are less than 0.005 millimetre; also a rock that is composed essentially of clay particles. Rock in this sense includes soils, ceramic clays, clay shales, mudstones, glacial clays (including great volumes of detrital and transported clays), and deep-sea clays (red clay, blue clay, and blue mud). These are all characterized by the presence of one or more clay minerals, together with varying amounts of organic and detrital materials, among which quartz is predominant. Clay materials are plastic when wet, and coherent when dry. Most clays are the result of weathering.