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it is a course-graind sediment and it belongs to the group of sediments that make up sedimentary rocks. Sand makes sandstones.

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Which does not belong shale limestone sandstone or basalt?

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).


What rocks are porous?

These are some porous rocks: chalk, limestone, sandstone, pumice, scoria.


Which does not belong shale basalt sand stone or limestone?

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.


Which types of rocks contains coal and petroleum?

Coal is typically found in sedimentary rocks such as sandstone, shale, and limestone. Petroleum is found in sedimentary rocks as well, usually in porous reservoir rocks such as sandstone or limestone that are capped by impermeable rock layers like shale or mudstone.


What are examples of rocks that are easily weathered and rocks re resistant to weathering?

Examples of rocks that are easily weathered include limestone, sandstone, and shale, which are sedimentary rocks. Rocks that are resistant to weathering include granite, basalt, and quartzite, which are igneous and metamorphic rocks that have a more crystalline structure and are less prone to chemical breakdown from weathering processes.