Valdivia, Chile

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Valdivia, Chile Website: http://www.chsbs.cmich.edu/luz_hurtado/chile-marcela/index.htm Requirements: Students must have completed at least SPN 341 and have a minimum GPA of 3.0 to enter this program. Students with a GPA below 3.0 but who are in good academic standing with CMU will be considered on an individual basis. Program: • This is an immersion program, which means that you will be taking courses taught in Spanish and your classmates will be Chilean students. • Classes are held at the Austral University campus in Valdivia. Class Schedule: • Semesters: o Session 1: February 23 through July 15 o Session 2: August 8 through December 15 o Classes are typically taught five days a week Course listing: • Desarrollo social de América Latina y Chile • Problemas y tendencias de la literatura hispanoamericana • La comunicación narrativa • Taller de redacción • Comunicación poética • Panorama de la literatura hispanoamericana • Seminario de literaturas alternativas • La comunicación dramática y teatral • Lexicología Española, etc. Teaching Staff: Classes are taught exclusively in Spanish by accredited native Spanish professors. Professors have MA and PHD degrees. Housing: Students will live and take their meals with a host family in the Valdivia area. Room and board costs approximately $2,000 for the semester. Possible trips you can take: You can ski in the natural refuges owned by the Universidad Austral in the Andes Mountains. You can visit Chascona, the house of the famous Nobel-prize winning writer Pablo Neruda. You can enjoy the thermal pools in Aguas Calientes in addition to natural parks, camping areas and cabins around the area. The Chiloé Churches in Chiloé (found in the UNESCO World Heritage list) are impressive architectural sites made entirely out of wood without the use of nails to hold them together. Another site of interest is the Mapuche Indian Reserve. Valdivia’s attractions: The botanic garden is one of the main attractions of the campus. Over 1,000 vegetable species, mainly native plants and trees from the south of Chile, are grown there. Surrounding the campus in the University Historical and Archeological Museum, a compulsory place to visit by people arriving to the tourist city of Valdivia. You can take a boat trip in the Calle-Calle River and look for sea lions. In Niebla you can visit the Spanish Fortresses, Playa grande, Playa chica and the Santuario de la Naturaleza (Nature Sanctuary), and look at the swans swimming in the river. Contact: Dr. Mary-Garland Jackson 313 Pearce Hall [email protected] .

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Crustal Deformation Associated with the 1960 Earthquake Events in the South of Chile
Paper No. CDDFV CRUSTAL DEFORMATION ASSOCIATED WITH THE 1960 EARTHQUAKE EVENTS IN THE SOUTH OF CHILE Felipe Villalobos 1 ABSTRACT Large earthquakes can cause significant subsidence and uplifts of one or two meters. In the case of subsidence, coastal and fluvial retaining structures may therefore no longer be useful, for instance, against flooding caused by a tsunami. However, tectonic subsidence caused by large earthquakes is normally not considered in geotechnical designs. This paper describes and analyses the 1960 earthquakes that occurred in the south of Chile, along almost 1000 km between Concepción and the Taitao peninsula. Attention is paid to the 9.5 moment magnitude earthquake aftermath in the city of Valdivia, where a tsunami occurred followed by the overflow of the Riñihue Lake. Valdivia and its surrounding meadows were flooded due to a subsidence of approximately 2 m. The paper presents hypotheses which would explain why today the city is not flooded anymore. Answers can be found in the crustal deformation process occurring as a result of the subduction thrust. Various hypotheses show that the subduction mechanism in the south of Chile is different from that in the north. It is believed that there is also an elastic short-term effect which may explain an initial recovery and a viscoelastic long-term effect which may explain later recovery. Furthermore, measurements of crustal deformation suggest that a process of stress relaxation is still occurring almost 50 years after the main seismic event. Keywords: tectonic subsidence, 1960 earthquakes, Valdivia, crustal deformation, stress relaxation INTRODUCTION Tectonic subsidence or uplift is not considered in any design of onshore or near shore structures.
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Important Dates Fall 2013 Study In: Fall General Information Meetings: Nov. 1, 2012, 5-5:50pm, Kidder 238 or Nov 7, 2012, 5-5:50pm, Kidder 238 ChillÁn, Winter Application Information Meetings: Attend either one January 17, 2013 or January 23, 2013 Chile hillán, Chile is a midsize town with a population C (location and times TBA) of about 150,000 located in central Chile, about 5 Application Deadline: hours south of Santiago. The climate and topogra- February 15, 2013 phy of the area are similar to those of the Deposit Due, Willamette Valley. Many are attracted to Chillán Non-Refundable: because of the great outdoor March 8, 2013 opportunities that it offers such Tentative Departure Date: as skiing (season June - Septem- September 3, 2013 ber), hot springs, and its many Tentative Program Dates September 3, 2013 - hiking possibilities. This univer- December 3, 2013 sity town is also located about an hour from the coast. The re- gion is named after the Bío-Bío Program Contacts river that runs through it. Foreign Languages & Literatures Lucía Robelo, Spanish Instructor he Universidad del Bío-Bío 541-737-3946 T (UBB) was founded on Sep- [email protected] tember 29, 1988, from the merger of the Instituto at the Profesional De Chillán and the Universidad de Bío- Laurie Wyant, Admin. Asst. / OS2 Universidad del Bío. The university contains two campuses: the Con- 210 Kidder Hall Corvallis, OR 97331-4603 cepción campus, in the region's capital, and the Bío-Bío Phone: (541) 737-3935 Chillán Campus, in the capital of the province of FAX: (541) 737-3563 Ñuble.
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