Basalt does not belong; it is an igneous rock and all the rest of them are sedimentary.
Sandstone, limestone, and shale are examples of sedimentary rocks. Granite, basalt, and obsidian are examples of igneous rocks.
Limestone, Sandstone, Shale
Conglomerate, limestone, sandstone, and shale.
Some examples of sedimentary rocks include limestone, sandstone, shale, and conglomerate. Limestone forms from the accumulation of calcium carbonate shell fragments, sandstone is made up of sand-sized mineral particles cemented together, shale consists of fine-grained clay and silt particles compacted over time, and conglomerate is composed of rounded pebbles or gravel held together by a matrix.
Some examples of lithified sediment are sandstone, shale, and limestone. Sandstone forms from grains of sand compacted together over time, while shale is formed from compacted clay and silt particles. Limestone is made predominantly of calcite that has accumulated and solidified in marine environments.
Limestone does not belong, as it is primarily composed of calcite, while the other three - shale, sandstone, and basalt - are all composed of different mineral compositions (clay minerals, quartz, and basaltic minerals, respectively).
In the question "which does not belong; shale, basalt, sandstone, or limestone?" the answer is Basalt. Shale, Sandstone, and Limestone are all sedimentary rocks. Basalt is an Igneous rock. Shale and Sandstone are both clastic sedimentary rocks which means they come from the "pieces" or remains of rocks after weathering. Limestone is a chemical sedimentary rock which means it is deposited as a result of a chemical reaction, or a collection of material made by organisms, such as coral. volcanic basalt dykes are molten basalt that rose through existing sedimentary rock, and crystallized when it rose to the surface about 32 million years ago. The magma cools and hardens which creats a basalt stack, resistant to weather. Basalt is a common extrusive volcanic rock.It color is usually gray or close to black.
Shale, sandstone, limestone, basalt, and granite are fairly commonly exposed on the surface of the Earth.
Sandstone, limestone, and shale are examples of sedimentary rocks. Granite, basalt, and obsidian are examples of igneous rocks.
Sandstone, Limestone, and Shale
Sandstone, limestone, shale.
Limestone, Sandstone, Shale
Sandstone, limestone, granite and shale.
limestone, sandstone, and shale
limestone, shale, and sandstone
These are sedimentary rocks. Sandstone is made of compressed grains of rock and sand. Shale is made of compressed bits of mud and clay. Limestone is made of compressed pieces of forms of calcium carbonate.
Shale, sandstone, and limestone belong to the sedimentary rock group. Sedimentary rocks are formed by the accumulation and compression of sediment over time. Shale is a fine-grained rock formed from clay and silt; sandstone is made up of sand-sized grains cemented together; and limestone is primarily composed of calcite from marine organisms.