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Recommended: My future plans
I am applying to the MSc degree program in Geology at the Department of Earth and Environmental Sciences, Ludwig Maximilian University of Munich, starting in winter 2014. My previous education and work experience as an exploration geologist make me a good candidate for this program. I have a strong research interest in understanding different Earth’s Lithosphere and plate boundary processes in relation to petrogenesis, mechanisms of rock deformation and metamorphism, and dynamics of crustal fluid migration during these deformation events through a combination of field-based, experimental and theoretical methods; with emphasis to better define and understand the architecture of fertile metallurgic districts. My future intent is to become an academia based consultant – structural geologist, in the mineral exploration industry. I found this programme appealing, as I believe that it can provide me with the necessary knowledge and competence to deal with the technical and theoretical shortcomings that are confronting me by offering a balanced coursework in deformation and transformation of rocks, tectonics, geochronology, ore geology, computer modeling and mathematical geology.
Some of the courses that I found very interesting while enrolled in the BSc degree program in Earth Sciences at the University of Asmara, include among others; igneous petrology and geochemistry. The theme of my topic for the course work “Literature review of geological topics” during my undergraduate studies was “Influence of hydrothermal fluids on silicate melts”. In hindsight, this experience allowed me to broaden my understanding on physical volcanology, hydrothermal systems and the mechanics of heat and mass transfer associated with hydrothermal fluid – se...
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...who can effectively bridge the gap between the knowledge rich academia and data rich industry. I am particularly keen to join this program as the department houses interesting faculty members actively engaged in research activities which predominantly coincide with my preferred research areas. In addition, I have gathered that, the Munich GeoCenter also houses interesting geophysics and geodesy research centers, which I can work with in a multi-disciplinary research projects. Besides the formal schooling, studying in the Federal Republic of Germany is important in its own right, for it can broaden my perspective and positively shape my future professional career. To top it all, it will present me with a chance to deepen my understanding of another culture, language and people. In reciprocity, I look forward to bring cross-cultural experience to the LMU student body.
Marshak, S. (2009) Essentials of Geology, 3rd ed. New York: W.W. Norton & Company, ch. 11, p. 298-320.
Riley, C.M. "Lahars." Geological and Mining Engineering Sciences. Michigan Tech. Web. 6 Feb. 2010. .
Tarbuck E., Lutgens F., Tasa D., 2014, An Introduction to Physical Geology, 5th Ed, Pearson Education, Upper Saddle River, New Jersey.
Plummer, C.C., McGeary, D., and Carlson, D.H., 2003, Physical geology (10th Ed.): McGraw-Hill, Boston, 580 p.
Smith, I. E. M., Price, R. C., Stewart, R. B., and Worthington, T. J. (2009). An assessment of the mantle and slab components in the magmas of an oceanic arc volcano: Raoul Volcano, Kermadec arc. Available: http://researchcommons.waikato.ac.nz/bitstream/10289/2685/1/Price assessment.pdf. Last accessed 10th Jul 2011.
Studying the effects of weathering and erosion on the uplifted and exposed basalt sill is important to understanding the geological events that lead to mass movements in the area. My researc sought to determine exactly what happens to a rock that has been exposed to natural weathering such as thermal, biological, chemical, and wet-dry also referred to as slaking, on a qualitative and quantitative scale. The weathering of the rocks, though apparent on the exterior of the sample, has an extreme and transformative effect on the internal structure (Gupta et al., 1999). Weathering disrupted the internal crystalline structure by producing microfactures, voids, and the deposition of clay minerals (Gupta et al., 1999). Basalt is heavily affected by weathering when concerning porosity and the formation of ...
The number of ancient extinct volcanoes for the tens of thousands; where there are volcanic rocks in most regions of the earth, and the significance of the volcanoes in the following:
The Saldania mobile belt comprises of structural features that are characterised by the occurrence of ductile and dextral strike-slip shearing that preceded the orogenic event which occurred approximately 600 Ma (Scheepers, 2000). This led to the first phase of magmatism about 560-540 Ma (Scheepers & Nortje, 2000). This phase involved the syn- to post tectonic S- type granites intruding the Tygerberg terrane (Scheepers & Nortje, 2000). The second phase involved the intrusion of the I-type granites. Like the S-type granites, the strike-slip movement affected the intrusion of the I- type granitoids which occurred along the Colenso fault in the Swartland and Boland terranes about 540- 520 Ma (Scheepers, 1995; Scheepers & Nortje, 2000). The intrusion of the post-orogenic to anorogenic A- type granites occurred at approximately 520- 500 Ma, representing the third phase of magmatism (Scheepers & Nortje, 2000). They are intrusive in the Tygerberg and Swartland terranes (Scheepers & Nortje, 2000). The final phase of magmatism is often negle...
Volcanoes are one of natures most interesting and dangerous phenomenons. The way volcanoes operate can be understood, on a basic level, by just some simple physics and chemistry, this paper will investigate and explain some of the basic physics that govern the behavior of volcanoes.
An exceptionally eminent faculty, an environment abounded with scholastic activity and a graduate program that beautifully blends the pearls of high-end course work and research facilities at the avant-grade of every field are the attributes that drive my motivation to choose your university for my graduate studies. I can affirm that I possess the basic aptitude, dedication and potential to maintain the aspiration and motivation required for my graduate study. I am certain that the graduate program offered by your University will prove to be the most efficient and effective approach towards my future career. I am convinced that this opportunity will significantly heighten my research expertise, providing me with the essential competence and allowing me to presume my knowledge and potentials to an advanced level.
Becoming a geochemist requires rigorous education and training in a variety of fields. For entry-level positions in geochemistry, a bachelor’s level degree is required in many majors, which take up at least four years of study. Many majors of choice of aspiring geochemists i...
Learning is a continuous process and the day that you stop learning is the day that you start decreasing your rewards and lower levels of satisfaction. My ardent desire to acquire knowledge has motivated me to pursue higher studies at graduate level, and to take up a career in research in industry. I have taken this decision after carefully considering my academic background, profound interest in research and strong aptitude for problem solving.
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...
My bachelor degree in Applied Geology led me to acquire a strong background of concepts such as structural Geology, Basics of Geophysics, Exploration Geophysics, Physics of the Earth and Petroleum geology. With extensive research and discussions with my professors and professionals linked with oil and gas industry, I chose Geophysics as my area of interest for my graduation.
the eruptive history of Somma-Vesuvius (1). Each was preceded by a long period of stillness, which in the case of the 79 A.D. eruption lasted about 700 years. These eruptions were fed by viscous water-rich phonotitic to tephritic phonolitic magmas that appear to have differentiated in shallow crustal conditions. They are believed to have slowly filled a reservoir where differentiation was driven by compositional convection. A minimum depth of about 3 km was inferred for the top of the magmatic reservoir from