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Senior Honors Theses

The Geology Department at Macalester College is committed to collaborative faculty-student research. To this end, many of our majors complete senior honors theses. A typical thesis-related research experience includes one or more summers of data collection and analysis (often in far-off places such as Crete, Zimbabwe, Mexico, Montana, Madagascar, and even southwestern Minnesota), followed by an oral defense and submission of a thesis to the library. In recent years, our students have conducted projects that focus on structural geology, geochemistry, paleontology, and sedimentology/stratigraphy.

The general requirements to participate in the Honors program may be found by clicking here.

Past Theses


   2009 (View Abstracts)
  • Rachel Murray
  • Hannah Wydeven
  • Alana Bartolai
  • Kenneth Nelson
   2008 (View Abstracts)
  • Danny Bowman
  • Robin Canavan
  • Sophia Kast
  • Alexandros Konstantinou
  • Scott Persons
  • Tom Tobin
   2006 (View Abstracts)
  • Cara L. Harwood
   2005 (View Abstracts)
  • Mara Brady
  • Chris Dwyer
  • Brett Dennis-Duke
  • Josephine Williams
  • Kirsten Fristad
   2004 (View Abstracts)
  • Anna Jerve
  • Brady Z. Foreman
   2003 (View Abstracts)
  • Michelle M. Casey
   2002 (View Abstracts)
  • Jennifer A. Anziano
  • Alexander W. McKiernan
  • Elizabeth A. Hajek
   2001 (View Abstracts)
  • Rebecca Terry
  • Travis O. Sandland
   2000 (View Abstracts)
  • Joshua Miller



Michelle M. Casey
Advisor: Ray Rogers
Senior Honors Thesis: 2003

Magnetostratigraphy of the Upper Cretaceous Maevarano and Berivotra Formations, Mahajanga Basin, Northwestern Madagascar

The Maevarano Formation and overlying Berivotra Formation cap the Upper Cretaceous section in the central Mahajanga Basin in northwestern Madagascar. The Berivotra Formation, which is marine in origin, yields an assemblage of fossils consistent with a Maastrichtian age (~65Ma). The age of the Maevarano Formation is presently based on correlation with the Berivotra Formation. In an effort to test and further refine the current age interpretations I analyzed the paleomagnetic signal from a suite of samples collected from both formations using alternating field demagnetization. The results show a long interval of normal polarity followed by a single reversal located in the uppermost part of the Berivotra Formation. This simple pattern could place this stratigraphic section any number of places within the global polarity time scale, but fortunately the Cretaceous-Tertiary Boundary provides an independent datum in the local section. Preliminary results of this magnetostratigraphic analysis suggest that the Berivotra Formation and the underlying Maevarano Formation are late Maastrichtian in age. Additional samples throughout the Maevarano and Berivotra Formations as well as a conglomerate test are needed to test the validity of this interpretation.


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