permeability
Because sandstone has wider particles than shale and this let's the water through.
Limestone, Sandstone, Shale
Sandstone is extremely porous and absorbs liquids like a sponge.. Shale is nearly impervious to liquids.
Clay turns into shale through compaction and cementation of fine clay particles, while sand turns into sandstone through the same process but with larger sand particles. Additionally, shale tends to have a more pronounced layering due to the smaller particle size of clay compared to sand, which results in a finer-grained texture in shale compared to sandstone.
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.
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.
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.
shale
Shale forms in layers of sandstone or lime.
a buried erosional surface
Because sandstone has wider particles than shale and this let's the water through.
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.
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
NO