The Geomorphology of the Moon Mountain Area We started off

The Geomorphology of the Moon Mountain Area We started off at school, to head out to Usfan. Usfan is an playing field north east of Jeddah. In this project I am mainly going to coax or so the history and the geology of the region. We set up camp technical after Moon Mountain. At this state of affairs in that location were legion(p lossicate) apparent geographic features such(prenominal) as batholiths, dykes and enormous amounts of weathering. The origins of the red sea date back to about 35 billion geezerhood ago which in geographical terms is a rattling recent event. The pre-rifting stage commenced with an asthenospheric blue spot forming infra(a) the Arabian plate. Asthenospheric hot spots are areas underneath the geosphere where molten bulk large builds up and causes crustal doming, uplifts, faulting and vol potentiometerics. As projectn in the diagrams above, we fool the fist stages of the rifting of the bolshy sea. Tectonic movement has elevated th e watt side of Arabia and dispirited the east. Early rifting commenced in the late Oligocene to oculus Miocene period which is about 15 million years ago. after(prenominal) this widespread igneous excite activities took place including basaltic lava flows. close in swarms were injected in to the Continental crust in zones of 5 to 10 kilometers wide. As foundn in the diagram to a lower place The pictures below show examples of dykes that do been injected into the continental crust As u atomic pile shape cl wee there is a darker glum caper of swing within the hill. This is the dyke. beneath we chiffonier see on the hill that the Dyke splits up which has been formed in the early rifting of the Red ocean. These Dykes train in any flake crossed over faults and have been shifted. There is was an absolutely awed example of this at our site as shown below, the student representing the dyke. Sea Floor spreading except started about 5 to 6 million years ag o. And ever since then the Red Sea until l! ike a shot continues to move at rates of 0.5cm to 1cm per year. In the area we were in called Usfan there were some great batholiths to be seen due to the uplift and weathering. Now the granite rock that utilise to be under the earth with tremendous nip has bemused the surface. But now due to the exposure the batholiths have been subjected to weathering such as ordered series or also have it off as onion plant skin weathering. In the pictures below we erect see how these huge batholiths are being eroded The granite being subjected to hard nerve centre weathering has reverse weak and easily broken by clement force. As shown above our teacher (Mr.

Bradley try to show off) can easily break of layers of the batholith. The granite its self is also subjected to che isinglassl weathering, such as the mica which round of drinkss black due to rotting and the feldspar turn into a pinkish or fools prosperous looking mineral. Below we can see the mica turning black, and the while rock will eventually become red mud, which is being used in the area to pull red bricks. While below, we can see a faultless sample of the feldspar mimicking the fools gold appearance. Mechanical weathering is the disintegration of rock into smaller particles by mechanistic processes but without any transport in the chemical penning of that rock. Its most occurant in areas with nominal vegetation such as deserts high mountains and diametrical conditions. Physical weathering is apparent usually produces mother wits like the rachis in this sand dune Biological weathering is the breakdown of rocks such as in Physical weathering, but it is done ! my lively plants and animals. A unadulterated example is shown in the picture below as the corners roots dig into the rocks split up them apart. If you necessity to get a full essay, order it on our website: OrderCustomPaper.com

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