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Sandstone

Adapted from Wikipedia · Discoverer experience

A beautiful sandstone building at The University of Sydney, showing its grand architecture and sunny courtyard.

Sandstone is a type of rock made mostly of tiny grains of minerals pressed together. These grains are about the size of sand, which is why the rock is called sandstone. It makes up about 20–25% of all the rocks formed from sand and mud.

Most sandstone is made from quartz or feldspar, minerals that stay strong even when weather wears them down. This rock can be many colors, like tan, brown, yellow, red, grey, pink, white, or black, depending on what other tiny bits are mixed in. Some famous places, like Arches National Park in the American Southwest, are known for their striking red sandstone cliffs.

Sandstone is special because it can let water flow through it and hold a lot of water inside. This makes it important for storing groundwater and oil deep underground. Over time, heat and pressure can change quartz sandstone into a different kind of rock called quartzite.

Origins

Sandstones are a type of rock formed from tiny bits of other rocks, called sand grains, that have been worn down by weather and movement. These grains are carried by rivers or wind to places where they settle and pile up. Over time, the sand grains get pressed together and stuck with a special glue-like material, turning into solid sandstone.

The process of turning loose sand into solid rock happens in stages. First, the sand is buried under more sand and sediment, which squeezes it tighter. Then, deeper down, heat and pressure help to glue the grains together. Finally, when the sandstone is closer to the surface again, water can dissolve some of this glue, making spaces inside the rock. This is how sandstone forms in nature.

Components

Framework grains are small pieces of rock, about the size of fine sand, that make up most of a sandstone. These grains are usually made of quartz or feldspar because these minerals stay strong even when weathered by wind, rain, or other natural forces.

Paradise Quarry, Sydney, Australia

Matrix is the tiny material found in the spaces between the grains. When there is very little matrix, the sandstone is called an arenite. When there is a lot of matrix, it is called a wacke.

Cement is a special material that sticks the grains together after the sandstone has formed. Common cements include silica, which is made of quartz, and calcite, which is a type of carbonate. Other minerals can also act as cement.

Pore space refers to the empty spaces between the grains in the sandstone. These spaces affect how much water the sandstone can hold and how easily water can flow through it. Porosity is the amount of space available, while permeability is how easily water can move through those spaces.

Types of sandstone

Sandstones are usually grouped by looking at very thin slices of the rock. This helps scientists understand what the rock is made of and where it came from.

There are different charts that help scientists figure out these details. Some charts show where the sand might have come from, while others show how the sand has changed over time.

Ternary plot showing the relative abundance of quartz, feldspar, and lithic grains in a sandstone

One way scientists classify sandstones is by the minerals they contain and the material between the grains. If a sandstone has less than 15% of this material between the grains, it is called an arenite. If it has more than 15%, it is called a wacke.

Sandstones can also be grouped by the types of grains they contain. Some have mostly quartz, some have more feldspar, and others have many different types of rock fragments.

When sandstone is changed by heat and pressure, it can turn into a rock called quartzite. In quartzite, the grains grow together and the rock breaks in a special way. Some sandstones can become very hard without turning into quartzite, and these are called orthoquartzites.

Uses

Sandstone has been used since ancient times for building, making art, and creating tools. People around the world have used it to build temples, churches, homes, and many other structures. It is also used in civil engineering.

Sandstone is easy to shape, which makes it popular for building and paving, like in asphalt concrete. However, some types of sandstone, like Collyhurst sandstone in North West England, don’t last well outside and need fixing or replacing in old buildings. Because of its hard grains and even size, some sandstones are great for making grindstones to sharpen blades and tools. Some sandstones without crumbling can also be used to grind grain, like gritstone.

The Main Quadrangle of the University of Sydney, a so-called sandstone university

Images

A stunning view inside Lower Antelope Canyon, showcasing its red sandstone corridors and natural beauty.
A close-up of a sandstone rock sample, showcasing its texture and mineral composition.
A natural rock formation showing layers of coal and sediment in Nova Scotia, Canada.
A beautiful rock alcove carved into sandstone near Moab, Utah.
Ancient sandstone tombs carved into rock in the historical city of Petra, Jordan.
Beautiful pink sand from Coral Pink Sand Dunes State Park in Utah.
A close-up view of layered rock formations showing cross-bedding and natural erosion patterns in Ohio.
A close-up of weathered rock formations known as grus, found in Great Basin National Park, Nevada.
A close-up view of volcanic rock examined under a microscope, showing its tiny crystal structure.
A scientific diagram showing how geologists classify sandstones based on their mineral content.
A beautiful 18th-century sculpture of the Virgin Mary in Freiburg, Germany.
An ancient sandstone oil lamp from the Magdalenian culture, found in the Lascaux cave and now displayed in the National Prehistory Museum.

Related articles

This article is a child-friendly adaptation of the Wikipedia article on Sandstone, available under CC BY-SA 4.0.

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