Senior Thesis Information

Senior thesis and the degree with honors

In order to be recommended for the degree with honors, a student is expected to have completed at least two semesters and a winter study project (031) of independent research culminating in a thesis that demonstrates outstanding achievement of an original and innovative nature. The principal considerations in admitting a student to a program of independent research are mastery of fundamental material and skills, ability to pursue independent study successfully, and demonstrated student interest and motivation.

Further advice on the major can be obtained from the department chair.

Recent Honors Theses


  • Biophysical Controls of Plum Island Estuary Tidal Channel Dynamics
  • 2019-2020 Atlantic Storm Season and its Impacts on Boulder Movement along Western Ireland
  • Conducting an Indoor Air Quality Analysis for Tallevast, Florida: A Majority Black Community facing TCE Contamination
  • Tephrochronology in the Aleutian Islands and Bering Sea: Assessing Tephra Correlations in Marine and Terrestrial Sediment Cores
  • Developing Digital Clast-Counting Methodology for Analysis of Boulder Beaches
  • What Drives CO2 Changes over Glacial-Interglacial Cycles? Controls on Nutrient Utilization & the Biological Pump in the Subarctic Pacific


  • Impact of the Length of Sea Ice-Free Summer Season on Alaskan Arctic Coastal Erosion Rates
  • Microfossils and Geochemistry of the Late Devonian Extinction Events in the Appalachian Basin
  • SKS Splitting Beneath Connecticut: Constraints from the SEISConn Array
  • sICEmic Sea Icea: Detecting Collisions with Seismology
  • A Dive into the Bering Sea: Reconstructing the Drivers of North Pacific Carbon Dioxide Flux Through Glacial-Interglacial Cycles of the Pleistocene


  • Impacts of Debris Flow on Landscape and Flood Risk in Coastal, Southern California
  • Unravelling the Role of Plants in Riparian Sedimentation: A Vegetated History of Avulsion on a Gravel-Bed River
  • Imapct of Summer and Fall Storms on Arctic Sea Ice Freeze-Up Timing
  • The Chronicle of an Oceanic Crust: The Tectonic Origin and Alteration History of Metabasalts Preserved on South Island, New Zealand
  • Geomorphology and Tectonism in Colorado’s Southern Front Range: Implications of Boulder and Volcanic Deposits on the Late Eocene Erosion Surface


  • How Can Storm Waves Move Very Large Boulders: Investigations in a Wave Tank
  • Photogrammetric monitoring of coastal boulder deposits
  • A Palynological and Geochemical Approach to Understanding the Late Devonian Kellwasser Events in the Appalachian Basin


  • Reconstructing Jökulhlaup Discharge Using the Morphology of Eroded  Volcanic Rootless Cones
  • A Reconnaissance Study and Interpretation of Enigmatic ca. 1.4 Ga  Plutons in the Southern Front Range, Colorado
  • Reinterpretation of Putative Tintinnid Lorica Fossils from the Tsagaan  Olom Group, Mongolia
  • Infiltration Variability and Shallow Groundwater Response to Snowmelt  in Headwater Catchments, Niwot Ridge, Colorado
  • From on High: Geochemistry of Alpine Springs, Niwot Ridge, Colorado  Front Range


  • The Water Balance and Hydrology of the Class of ’66 Environmental Center
  • Modeling Non-Linear Storm Wave Behaviour for Coastal Boulder Transport in the Aran Islands, Ireland
  • Changes in Sediment Transport and Present-Day Carbon Storage Due to Historic Charcoaling Activity in Litchfield, CT
  • Not Just Flowers: Vases in the Neoproterozoic
  • Tiny Fossils from a Big Extinction: Microfossil Assemblage Variation Through the Kellwasser Event of the Late Devonian
  • The Geomorphology of Mountains on Io
  • Detrital Zircon Constraints on the Age of the Granville Dome Mantling Sequence
  • Tephronchronology as a Tool to Constrain Surface Reservoir Ages in the Deglacial Bering Sea


  • Comparison of Icelandic Rootless Spatter Cones with Experimental Lava Features
  • Connecting Surficial Deposits and Hydrologic Flux in Leaky, Snowmelt-Dominated Catchments, Niwot Ridge, Colorado
  • Geomorphic Effects of the September 2013 Flood in Fourmile Canyon, Colorado, Using Lidar and Field Studies
  • Boulder Movements in Western Ireland