Is Sandstone Older Or Granite

Though some rocks look identical they have certain characteristics which distinguish them from others.

Is sandstone older or granite.

Arkose sandstone is one type of immature sandstone. 1 july 2013 at 16 35 the schist is older. It can form as basal sandstone from granitic coastal areas or can be found in faults and low areas adjacent to granite mountains ch 5 pg 99. This natural material can be finished in a number of ways.

Most sandstone is composed of quartz or feldspar both silicates because they are the most resistant minerals to weathering processes at the earth s surface as seen in the. Inclusions are always older than surrounding country rock. Of immature sandstone mostly quartz however have an abundance of other minerals such as feldspar mica chert and rock fragments. Sandstone is a clastic sedimentary rock composed mainly of sand sized 0 0625 to 2 mm mineral particles or rock fragments clasts or organic material.

Other minerals clays hematite ilmenite feldspar amphibole and mica and small rock fragments lithics as well as organic carbon bitumen add color and character to the clastic fraction or the matrix. Also the juxtaposition of a met rock with ig rock meta rock had to be in place first dead giveaway. Like granite and marble sandstone is mined and cut from solid stone. Sandstones make up about 20 to 25 percent of all sedimentary rocks.

I think it s pretty obvious that the schist is older the granite seems to cut the metamorphic foliation. Basalt vs sandstone characteristics assist us to distinguish and recognize rocks. Depending on the properties like hardness toughness specific heat capacity porosity etc rocks are resistant to heat wear impact etc granite is heat resistant wear resistant whereas sandstone is heat resistant impact resistant pressure resistant. Then later a new pluton cooled creating new granite that is younger than the sandstone.

Basalt vs sandstone characteristics. But you could have had an igneous rock millions of years ago that was weathered and eroded into sediments that then became the sandstone. Mature continental sediment consists of a handful of surface minerals and sandstone therefore is usually almost all quartz. Granite is extremely hard and less affected by the freeze thaw cycle the forces of abrasion and the surface exfoliation processes that are all a part of physical weathering.

Then the sandstone could be weathered and eroded itself into a new sandstone unit that is younger than the new granite. Incredibly hard granite is used in building masonry projects where it was originally quarried see the red and pink areas of the map notably aberdeen and cornwall. This natural material can be finished in a number of ways. The specific heat capacity of granite is 0 79 kj kg k and that of sandstone is 0 92 kj kg k.

Characteristics of rocks include texture appearance color fracture streak hardness etc.