T180 International Research Experiences for Undergraduates (Posters)

Tuesday, 2 November 2010
8:00 AM - 6:00 PM
Hall D

TRADITIONAL GEOLOGY FIELD CAMP: A CAPSTONE COURSE AT BLACK HILLS NATURAL SCIENCES FIELD STATION (SDSMT)

Paper number: T180-2
Program: Technical Sessions
Time: 8:00 AM – 6:00 PM

Authors

Abstract

The Black Hills Natural Sciences Field Station has provided field training in geology and geological engineering for more than 40 years, and since the 1980’s as a consortium serving five schools with South Dakota School of Mines and Technology as the coordinator. The traditional summer geology field camp is a five week long, intense program aimed to prepare students for subsequent professional geologic experiences. It is delivered from two separate facilities, one in the Black Hills (South Dakota) from a beautiful log lodge along Sand Creek, in eastern Wyoming, and a second from the town of Taskesti along the North Anatolian fault approximately 200 km east of Istanbul, Turkey. At both locations, the courses maintain a strong emphasis on basic field applications, including the use of GPS as a mapping tool in most exercises. The preparation of well-written reports, based on field descriptions supplemented by research on the web or through published documents, is strongly emphasized.

Projects at the Black Hills field camp includes mapping of Precambrian basement, Paleozoic stratigraphy, and Laramide Tertiary plutons and structural features as welll as post-Laramide,, faulted continental strata. The popular Taskesti field camp utilizes the diverse geology of the Tethyan realm, as well as the culture and history, of central Turkey (Anatolia). The course is based at a Turkish Government Earthquake Research Center facility along the North Anatolian fault. Students examine and map selected locations across the Izmir-Ankara suture including: 1) Deformed Cretaceous and Tertiary carbonate and clastic strata of the Sakarya micro-continent in a fore-arc basin; 2) Marble and skarn surrounding Eocene, subduction-related granite intruded into a passive margin sequence in the Sivrihisar region of central Anatolia; 3) Faulted and folded Neogene strata in the northern flank of the post-Tethyan, Haymana Basin and the contrasting terrains across the North Anatolian fault (J/K carbonate and clastic strata juxtaposed against amphibolite grade metamorphic and ophiolitic complexes)

Student comments during and after field camp support full immersion into a traditional summer geology field camp as an unforgettable experience (life changing in some cases) -- everyone who dreams to be a geologist should have a chance to taste it.