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Sedimentary rocks ____
Sedimentary rock ____
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Sedimentary rocks are the rocks formed from compaction and cementation of fragments of pre-existing rocks called crystals. Exogenic processes such as weathering and erosion influence the formation of sedimentary rocks. This processes supply the materials (sediments), responsible for the formation of sedimentary rocks. Weathered materials are transported by the agents of denudation such as water, wind and ice; then are deposited in low altitude areas. The accumulated materials are compacted as results of increasing pressure, finally the material are cemented following the precipitation of silica, calcium carbonate or iron oxide between particles. Sedimentary rocks are formed in layers through the process called stratification, the layers formed are called strata. Usually the old rock strata underlie the young rock strata. The more you go deep, the older rock it becomes unless there is an abnormal. Fig 1: show strata of sedimentary rocks. Sedimentary rocks can be classified into two major categories namely, clastic and non -clastic sedimentary rocks. Clastic sedimentary rocks, according to Astrahler clastic sedimentary rocks are the rocks derived directly as particles broken from the parent rock source. Clastic sedimentary rocks are derived from any one of the rocks groups which are igneous rocks, sedimentary rocks or metamorphic rocks which gives a way wide range of parent materials. Clastic sedimentary rocks vary in size of particles from fine particles to courser particles, for instance from siltstone, sand stone to conglomerates which is formed by the compaction of large pebbles. Non- clastic sedimentary rocks , this the type of sedimentary rocks formed of newly created mineral matt... ... middle of paper ... ...trary to non-clastic sedimentary rocks which are less denser for instance dolomite and anhydrite. Non-clastic sedimentary rocks especially organically formed sedimentary rocks are responsible for forming crude oil and gas after millions of years where as Clastic sedimentary rocks form inorganic substances such as rocks including silt stone , sand stone , clay stone and conglomerate. However the two types of sedimentary rocks are all important to the nature. for instance clastic rocks provide building material like sand , Organically sedimentary formed rocks provided fuel such as coal, petroleum and natural gas .Also chemically formed sedimentary rocks provide rocks salt after precipitation . More over sedimentary rocks forms recreational resorts, like reefs and island .
The Kimmeridge Clay Formation is the penultimate formation of the onshore British Jurrasic Succession. William Smith was the first to document this distinct formation on his map of 1815, and to name as the Oaktree Soil. In 1817, he gave the name Oaktree Clay for the layers of clay between the “Portland Rock” and “Coral Rag and Pisolite” but in 1816 Webster was the first to describe in details the formation and changed to the name now known as kimmeridge Clay Formation after the English village of Kimmeridge on Dorset’s “Jurassic Coast” a place frequently visited by fossil hunters. (Cox and Gallois, 1981).
The shelf-edge includes carbonate-to-clastic facies transition and tectonic uplift and erosion of the carbonates followed by deposition of the clastics. The Saint Peter Sandstone is a well-sorted, almost pure quartz arenite deposited during a major mid-Ordovician low stand. Clastics spread across an exposed carbonate platform by transportation. This is shown by the well-rounded, frosted texture of the quartz grains.
The Don Valley Brickwork consists of many different layers of geological deposits, allowing us to observe and have a better understanding of how the sediments we see today are formed. The most bottom layer in the Brickworks are from the Georgian Bay Formation, and consists of grey- shale bedrocks. Fossils are often found in this layer and it is estimated that this deposit of sediments is around 445 million years old. Above the bedrocks is a thin layer of grey clay sand and gavels left behind by the Illinoian Glacier. This layer is called the York Till and occurred around 135,000 years ago. The next layer consists of a sandy deposit called the Don Formation, which is formed by the Sangamonian Interglacial Stage. Many plant and animal fossils are found in this layer due to warmer climate around 120,000 years ago. Above it lies the Scarborough Formation, which consist of clay and sand. This sediment likely occurred 115 - 106,000 years ago. The next layer above is the Poetry Road Formation, and consist of sand and gravel. This layer is likely formed during the early Wisconsin glacial substage around 106- 75,000 years ago. Higher is the Sunnybrook Drift which was formed 60 – 75,000 years ago. And on the surface, is the Halton Till, which was left behind by the final push of the Wisconsin Glacier.
Quartzite is a non-foliated metamorphic rock. This rock is intrusive and forms when exposed to extreme amounts of heat and pressure. Over a billion years ago, there was an ocean where Kamiak Butte is. This ocean floor was made of sand, as time went on oceans receded and the exposed sand underwent processes that turned it into sandstone – or as we learned in class the process of lithification. Years later, this sandstone would morph into the quartzite that is present now.2
Soon after the sea reached longer distance westward and the sandy tidal deposits were converted to deep water deposits. Mancos Shale is the name given to represent these deposits, which are comprised of organic material and small particulates. Another interesting fact to note is that this type of sediment consists of fossils. These remains can include prehistoric shell fish, shark teeth, and many other types of organisms. The hills seen at the foundation of the mesa in the Montezuma Valley are comprised of gray
This sedimentary rock has hardened over the many years with sand shells, small pebbles, grains of sand and rocks of various sizes. In comparison to our 4.5 billion year old Earth, these sand shells might as well be brand new, when in reality they could be up to 1,000 years old. If the sandstone were to be replaced with calcite it would completely change the subclass of rock, it would then be chemical & organic limestone. The variation in sand stone is due to different rates of deposition and change in patterns of the sediment movement (Mc Knight, p. 384). These tightly compacted varying stones and shells will be weathered away by wind and waves over time and could eventually be reduced to a rock the size of your hand.
"Sedimentary Rocks." Backyard Nature with Jim Conrad. N.p., 18 May 2015. Web. 25 Oct. 2015.
...These rocks include indurated conglomerates, coarse-grain granites, and Arkosic and breciated granites. Furthermore, there are evidences to indicate that faulting took place in the area. Hydrothermal and epithermal action must have intruded the rocks in the Goldfield area forming small stringers of quartz. There are also evidences of sedimentary rocks such as sandstones, limestone and conglomerates found near Roosevelt Lake (Eppinga, 2006).
At the base there is a dry creek bed of granite that has been cut by a series of fractures. Fine black rock along these fractures is called gouge. Fault gouge is comprised of little pieces of rock that was ground upward when the fault moved. Once you go up the trail and climb past the trees to the large space of bare rock, you are on the exfoliation dome. At this point you can examine the “coarse-grained porphyritic granite that makes up the majority of Enchanted Rock”. As you examine the surface, you will see how the granite magma cut into the surrounding rocks. When this occurred over a billion years ago, the magma was a combination of very hot liquid and crystals. Once you reach the mid-point of the climb you can see to your right a boulder-covered granite hill known as “castle tor”. An area on the rock that looks like a line down the slope is called an aplite dike. Several of these cut the rock; these consist of fine-grained granite with a sugary texture and minimal biotite. Dike describes the crack where molten rock has been inserted. As you climb up the front, a section of rock has a texture change. This appears to be a Ductile Shear Zone, a long narrow change that has a more fine grain consistency.
regions of the earth can indicate which rock layer is older than the other. Trilobite fossils
Colorado is home to eleven national parks, with different stories to be told in each one! One of those parks is the Rocky Mountain National Park. In this park alone you can find all three rock types of all ages. For example, there is Silver Plume granite that “intruded upward into the metamorphic rocks about 300 million years after the formation of the Proterozoic mountains” and can be found in the eastern side of the park (“Geology resources division,” 2007). Geologist are unsure what caused this
Paleogeologist knows a fossilization process only begins when an organism dies and immediately covers with mud or silt before it gets ruined by scavengers. After being covered under earth’s surface, minerals in the water replace the minerals in the organism’s tissues, and bones are the most common tissues for mineral replacements. Because the soft parts of the body usually decays and left with the hardest parts to be buried. After much time has passed the body of the organism will slowly turn into a sedimentary rock. This process would sometimes take up to millions of years; therefore fossils do not form easily.
The layer can be buried under other layers of sediment. After a long time the sediments can be cemented together to make sedimentary rock. In this way, igneous rock can become sedimentary rock. All rocks can be heated. But where does the heat come from?
Some mountains start at the bottom of the sea. Scientists found that out when they took limestone off Mt. Everest and found dead sea creatures. Limestone is a kind of rock that is formed very slowly over thousands of years. Animals and plants that get stuck in limestone are called fossils. Limestone and fossils are common in most mountains that originate at the bottom of the sea.
The field of geology has many different branches. Some of these areas have hardly anything in common. The one thing that they all include, though, is that each one concentrates on some part of the Earth, its makeup, or that of other planets. Mineralogy, the study of minerals above the Earth and in its crust, is different from Petrology, the st...