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The Universities of Exeter, Bristol, Bath, Plymouth and UWE Bristol have created the South West Doctoral Training Partnership (SWDTP) which draws together the established research excellence of academic and research staff at the five institutions. As part of the MPhil/PhD Sustainable Futures programme you will have supervisors from more than one discipline and more than one institution. Your home institution will be wherever your lead supervisor is based. Thus you will be able to benefit from the expertise of staff from a much wider base than is usual. In western India, the Kutch region in Gujarat and Koyna in Maharashtra are classified as a Zone IV region (high risk) for earthquakes. The Kutch city of Bhuj was the epicentre of the 2001 Gujarat earthquake, which claimed the lives of more than 1,337 people and injured 166,836 while destroying or damaging near a million homes. [39] The 1993 Latur earthquake in Maharashtra killed 7,928 people and injured 30,000. [40] Other areas have a moderate to low risk of an earthquake occurring. [41] Coastal plains Visakhapatnam beach view, Bay of Bengal, Andhra Pradesh. Varkala beach on Kerala's coast, Arabian Sea
You can start in September, January or April but we strongly encourage a you to enrol in Term 1 in September as induction events are focused around this start date. However, we do permit MSc by Research/MPhil/PhD students to enrol either at the start of Term 1, Term 2 or Term 3 (see the University's term dates), or on the 1st of any other month except August, September and October. Requirements for international students The programme gives you the flexibility to shape your own research in an area of particular interest to you. Like other research degrees you will be required to work independently, but with the support and guidance of an appropriate supervisor. Bruun, P., 1954. Coast erosion and development of beach profiles. U.S. Army Corps of Engineers. Beach Erosion Board, Technical Memorandum No. 44.of our students are in employment or further study within 15 months of finishing their studies (HESA Graduate Outcomes, 2019/20) Severity of coastal flooding can be determined by considering the properties that would be affected by flooding, especially their economic value or worth if damaged. The entry grades outlined in this section indicate the likely offer or range of offers which would be made to candidates along with any subject specific requirements. This is for general information only. Keele University reserves the right to vary offer conditions depending upon a candidate’s application. Read more about our undergraduate entry requirements. Naunidhi Kaur (June 2002). "The Nowhere People". Frontline Magazine, the Hindu. 19 (12). Archived from the original on 8 December 2008 . Retrieved 19 November 2008. {{ cite journal}}: CS1 maint: unfit URL ( link) Further along the long profile, the cross-valley profile becomes widened and deepened by a combination of lateral and vertical erosion. Rivers in the middle and lower course are characterised by an increase in discharge and this gives the water the (kinetic) energy to erode the riverbed and banks further. There is an excess of energy available due to more efficient usage (channel bed roughness is reduced so less energy is absorbed overcoming friction) and this is used by the river to erode laterally, producing a much wider valley bottom with side slopes which are well separated. In addition, with the decrease in gradient associated with the lower reaches of a river comes an increase in deposition, and this leads to the formation of wide floodplains and levees either side of the channel Further influences on cross-valley profiles
We offer a personalised learning experience in an environment where you can feel part of a community. All the Geography team at Keele, including world expert researchers in their field s , are involved in teaching on this programme so you will be working closely with people who, “wrote the book” on your subject area.
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iii) Rating – ask participants to rank a small number of categories from most important to least important. Use a set of graduated sieves can be used to sort sediment samples into different size categories (in millimetres or as phi sizes).
The Himalayas act as a barrier to the frigid katabatic winds flowing down from Central Asia. Thus, northern India is kept warm or only mildly cooled during winter; in summer, the same phenomenon makes India relatively hot. Although the Tropic of Cancer—the boundary between the tropics and subtropics—passes through the middle of India, the whole country is considered to be tropical. [77] Temperature averages in India; units are in degree CelsiusThe Ganges- Brahmaputra- Meghana system has the largest catchment area of about 1,600,000km 2 (620,000sqmi). [61] The Ganges Basin alone has a catchment of about 1,100,000km 2 (420,000sqmi). [30] The Ganges originates from the Gangotri Glacier in Uttarakhand. [60] It flows southeast, draining into the Bay of Bengal. [30] (The Yamuna and Gomti rivers also arise in the western Himalayas and join the Ganges in the plains. [30] The Brahmaputra originates in Tibet, China, where it is known as the Yarlung Tsangpo River) (or "Tsangpo"). It enters India in the far-eastern state of Arunachal Pradesh, then flows west through Assam. The Brahmaputra merges with the Ganges in Bangladesh, where it is known as the Jamuna River. [30] [62]
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