Because sandstone has wider particles than shale and this let's the water through.
Shale largely consists of overlapping platy clay minerals which makes it fairly impermeable. With sandstones rounded grain texture, the gaps between the grains make it permeable.
Because sandstone has wider particles than shale and this let's the water through.
Spaces between shale are so small that water cannot pass through them. Because the cementation process does not fill all the the spaces between sand grains, sandstone contains many small holes.
Because sandstone has wider particles than shale and this let's the water through.
Water has great difficulty seeping through shale because shale is non porous. While shale is brittle, it has a very dense quality.
Sandstone is extremely porous and absorbs liquids like a sponge.. Shale is nearly impervious to liquids.
The sandstone acts as a filter, stopping impurities and dirty, etc. from passing through.
because sandstone is a porous media meaning it have a lot of pores then mud filtrate (its water) can enter the rock but the solids of the mud cant hence mud cake form.shale is a porous media too but its pores not connected together so mud cant enter the shale and mud cake don't form.
sedimentary rocks~ types of rock that are formed by the deposition of material at the Earth's surface and within bodies of water and some examples are limestone, conglomerate, sandstone, and shale
No, sandstone is not soluble in water.
Quartzite
Because shale and sandstone don't let water pass them, but conglomerate does
shale is metamorphic, which means time, pressure and temperature has altered it. Sandstone is sedimentary which means it was formed under water. generally sandstone is younder.
No. Not that well as sandstone. The shale starts to puddle into the water and flows inside the small puddle of water.
"The two basic rocks found in the Mammoth Cave area are limestone and sandstone. Limestone is the "soft" rock (more water soluble) that is dissolved more easily by water. Sandstone and shale are the rocks that are on top of the cave. They are "harder" (less water soluble) and don't let the water soak into the cave." http://www.nps.gov/archive/maca/learnhome/cur_k3_cla.htm
granite
Sandstone is extremely porous and absorbs liquids like a sponge.. Shale is nearly impervious to liquids.
Because sandstone, silty shale, and shell limestone usually have origins of formation on or near shore, the pebble conglomerate is left. Pebble conglomerates are formed from deposition of water transported rocks of larger size than the smaller rock particles which compose sandstone and shale. The larger size indicates they were transported and deposited further from the shoreline.
Basically, it's iron rust. Pure sandstone is white, and water can very easily seep through this rock. When the water meets or carries iron into this rock, the iron rusts and becomes red.
Shale
Limestones are form by precipitation of rusually under water Sandstones are formed from sendiments that are being eroded and compacted and cemented together. Shale are formed from precipation also but you often see fossil records on them.
The sandstone acts as a filter, stopping impurities and dirty, etc. from passing through.