No. Shale forms from clay and silt, which are much finer than the sand that forms sandstone.
Hermit Shale is a layer of sedimentary rock found in the Grand Canyon that is older than the Coconino Sandstone. Hermit Shale is made up of clay, silt, and sand, while the Coconino Sandstone is composed of cross-bedded sandstone. The Coconino Sandstone is also known for its distinctive frosted appearance due to the quartz grains it contains.
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.
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).
Hermit Shale is a sedimentary rock composed of clay and silt, while Coconino Sandstone is a sandstone rock composed of sand grains. These two rock formations represent different depositional environments, with Hermit Shale indicating a slower and gentler deposition compared to the Coconino Sandstone's faster and more energetic deposition.
The resistivity of sand can vary widely, but generally ranges from 1,000 to 10,000 ohm-meters. Sandstone typically has a resistivity of around 1 to 100 ohm-meters. Shale generally has a resistivity of 0.1 to 10 ohm-meters.
Hermit Shale is a layer of sedimentary rock found in the Grand Canyon that is older than the Coconino Sandstone. Hermit Shale is made up of clay, silt, and sand, while the Coconino Sandstone is composed of cross-bedded sandstone. The Coconino Sandstone is also known for its distinctive frosted appearance due to the quartz grains it contains.
shale
Shale forms in layers of sandstone or lime.
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.
Quartzite
Limestone, Sandstone, Shale
Sandstone, Limestone, and Shale
permeability
Sandstone, limestone, shale.
NO
Sandstone is extremely porous and absorbs liquids like a sponge.. Shale is nearly impervious to liquids.
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).