Sedimentary rocks are one of the incredible secrets that lie beneath your feet. They are members of the three primary families of rocks on Earth. They appear in more places than you might think, but we hardly ever give them much thought. Sedimentary rocks include the coal used to power homes and the sand on the beach. These rocks took thousands of years to accumulate every layer. Although they may appear unremarkable at first, they are essentially nature's journal, documenting the lengthy history of the planet. So let's examine what makes them noteworthy.
Imagine a river flowing across the environment, gathering little stones, dirt and sand. All of that stuff has to land somewhere and it does; it sinks to the bottom of lakes, rivers, or the ocean. As the years pass, more material keeps piling on top. The upper layers push down hard on everything below them. Give it enough time, we're talking thousands of years and those squished-down layers eventually go solid. That's your sedimentary rock, right there. The particles that sink and settle are called sediments, which is exactly where the rock gets its name.
Sedimentary rocks take up roughly 75% of the Earth's land surface. This indicates that sedimentary rock makes up the majority of the ground you walk on every day. Sometimes it just appears to be flat slabs of sand, clay, or striped stone; you might not even recognize it as rock.
Finding the layers of a sedimentary rock, which scientists refer to as strata, is the simplest way to identify it. Each layer was developed at a distinct time. The more recent layers are at the top and the older material is at the bottom. Scientists are able to piece together what Earth looked like millions of years ago by reading these strata as if they were a book.
The majority of fossils found in museums were extracted from sedimentary rocks. This is because sediment can swiftly bury a dead plant or animal near water before it completely decomposes. It becomes trapped inside the hardening rock over an extended period of time and becomes a fossil. For this reason, experts researching ancient life find these rocks to be extremely valuable.
Sedimentary rocks aren’t all the same. They fall into three groups:
Sedimentary rocks are useful to humans in a variety of ways; they don't just sit there looking ancient. Limestone goes into making cement. Coal keeps our lights on and our homes warm. Rock salt ends up in our kitchens. And petroleum, the stuff that gets refined into petrol and diesel, sits trapped between deep layers of sedimentary rock underground.
There's no rushing this process. It takes hundreds of thousands to millions of years for sediments to pile up thick enough and press together hard enough to become actual rock. The rocks sitting around us today started forming long before the first human being ever walked the Earth.
In India, sandstone is probably the most familiar sedimentary rock. Red sandstone was used in the construction of some of the nation's most famous historical buildings, such as Delhi's Red Fort. Because it is durable, simple to shape and actually attractive, builders have always adored it.
Sand, mud, clay, shells and fragments of other rocks make up sedimentary rocks. Over time, these fragments form layers, gradually condense and solidify as rock.
They are found near rivers, lakes, oceans and deserts. They cover a huge portion of the Earth's surface and are probably the most common type of rock most people ever come across.
Fossils need the right conditions to form; mainly, something needs to be buried under sediment quickly and then left undisturbed for a very long time. Sedimentary rocks offer exactly that. The other two rock types, igneous and metamorphic, form under intense heat or pressure, both of which would destroy any fossil before it ever had a chance to form properly.
Layers of settled material give rise to sedimentary rocks. Magma, or molten rock, originates deep inside the Earth and cools to form igneous rocks. Older rocks that were altered by the intense heat and pressure found deep beneath are known as metamorphic rocks. Each one has a very distinct appearance and forms in an entirely separate habitat.
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