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Sandstone is extremely porous and absorbs liquids like a sponge.. Shale is nearly impervious to liquids.
Because sandstone has wider particles than shale and this let's the water through.
Sandstone is a sedimentary rock.
permeability
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.
Sandstone is extremely porous and absorbs liquids like a sponge.. Shale is nearly impervious to liquids.
shale
Shale forms in layers of sandstone or lime.
No, shale and sandstone are two distinct types of sedimentary rocks. Shale is composed of very fine-grained particles, while sandstone is composed of sand-sized grains that are visible to the naked eye.
Because sandstone has wider particles than shale and this let's the water through.
Sandstone is typically older than shale, as sandstone forms from the consolidation of sand particles through compaction and cementation, while shale forms from the compaction of clay and silt particles. Sandstone is generally associated with sedimentary environments that occurred earlier in geological history compared to those where shale forms.
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.
Quartzite
Sandstone is a sedimentary rock.
NO
Sandstone, Limestone, and Shale
Sandstone, limestone, shale.