a sandstone would break more easily because a quartzite is harder. a quartzite is made of sandstone melted together by magma
Sand would likely metamorphose into quartzite, a metamorphic rock made predominantly of quartz. Sand is primarily composed of quartz grains, and under heat and pressure, these grains can recrystallize and compact to form quartzite.
It would be highly unlikely. When a rock undergoes metamorphasis the minerals in the sample often move small distances and aggregate with others of its kind. This process would obliterate the traces of fossils in most instances.
A brittle material is one that fails by fracturing after only a very small amount of plastic strain has occurred. Sandstones tend to be made up of quartz and feldspars which are themselves brittle. However sandstone and many other materials are only thought of as brittle because we are used to dealing or working with them at the pressure and temperature conditions present at the Earth's surface and can actually be either brittle or ductile (significant plastic deformation can occur before ultimate rupture) depending on the temperature, confining pressure and strain rate applied to it. In general at low confining pressures and temperatures (i.e. near the Earth's surface), sandstone will fail in a brittle fashion. However as the temperature and or confining pressure increases it becomes increasingly ductile.
To find an aquifer, you would typically need to look for rocks that are porous and permeable, such as sandstone, limestone, or fractured volcanic rock. These types of rocks allow for the movement and storage of water within their spaces, forming potential underground reservoirs from which water can be extracted.
As the water froze and expanded, it would exert pressure on the surrounding sandstone. This pressure could cause the sandstone to crack or fracture, as the ice expands and pushes against the rock material. Over time, repeated freezing and thawing cycles can lead to weathering and erosion of the sandstone.
Sandstone
In quartzite the grains are essentially welded together under pressure, which holds them together much more strongly than the fairly weak cementation in sandstone.
The new rock formed after the recrystallization of quartz sandstone is called quartzite. This process involves the metamorphism of sandstone under high pressure and temperature conditions, resulting in the formation of quartzite, which is a harder and more compact rock than its precursor.
sandstone or quartzite is very hard stone i think there is no possibility that it can form a soil....because if undergo weather cycle it only form igneous rocks which is smaller and less harder than the original properties
The metamorphic rock quartzite would form due to the heat and pressure.
Quartzite is already a metamorphic rock formed from sandstone under high pressure and heat. It does not transform into another mineral due to pressure and heat.
Sand would likely metamorphose into quartzite, a metamorphic rock made predominantly of quartz. Sand is primarily composed of quartz grains, and under heat and pressure, these grains can recrystallize and compact to form quartzite.
it looks like a stone made out of sand and it brakes easily.
Quartzite is a metamorphic rock, which means it was once a different type of rock (such as sandstone) that underwent intense heat and pressure to form quartzite. It is composed primarily of quartz grains.
Sandstone is more easily eroded than lava.
It would be highly unlikely. When a rock undergoes metamorphasis the minerals in the sample often move small distances and aggregate with others of its kind. This process would obliterate the traces of fossils in most instances.
The presence of visible minerals aligned in bands or layers would distinguish schist and gneiss from quartzite and marble. Schist and gneiss show foliation due to intense metamorphism, while quartzite and marble are more homogenous in texture.