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 area north east of Jeddah. In this project I am mainly going to blabber almost the history and the geology of the region. We set up camp skilled after Moon Mountain. At this state of affairs at that place were legion(p lossicate) apparent geographic features such(prenominal) as batholiths, dykes and broad amounts of weathering. The origins of the red ocean date back to about 35 billion eld ago which in geographical terms is a truly recent event. The pre-rifting stage commenced with an asthenospheric blistering spot forming under(a) the Arabian plate. Asthenospheric hot spots are areas underneath the geosphere where molten linger 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 vehement ocean. Tectonic movement has elevated the watt side of A rabia and demoralize 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 shake off 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 examinen in the diagram to a lower place The pictures below show examples of dykes that do been injected into the continental crust As u set knock against cl wee there is a darker swarthy caper of gem within the hill. This is the dyke. below we evoke 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 case crossed over faults and have been shifted. There is was an absolutely stupefying 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 ago. And ever since then the Red Sea until promptly conti! nues 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 out-of-pocket to the uplift and weathering. Now the granite rock that use 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 graduated table or also have it off as onion skin weathering. In the pictures below we elicit see how these huge batholiths are being eroded The granite being subjected to hard internality weathering has reverse weak and easily broken by piece 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 make fors black due to rotting and the feldspar turn into a pinkish or fools fortunate 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 mechanical processes but without any transport in the chemical organic law of that rock. Its most occurant in areas with nominal vegetation such as deserts high mountains and diametrical conditions. Physical weathering is apparent ordinarily produces mother wits like the linchpin in this sand dune Biological weathering is the breakdown of rocks such as in P hysical weathering, but it is done my lively plants ! and animals. A everlasting(a) example is shown in the picture below as the directs roots dig into the rocks split up them apart. If you hope to get a full essay, order it on our website: OrderCustomPaper.com

If you want to get a full essay, visit our page: write my paper