Examination of the genesis and evolution of magmas in various tectonic environments of the Earth, approached through theoretically and experimentally derived phase equilibria of liquid/crystal systems, isotopic relationships, trace and rare earth element geochemistry, and case studies of naturally occurring igneous systems. Prerequisite: Geo-Sci 321.

This seminar explores the skills, resources and habits that help Geosciences graduate students to succeed in graduate school and in their careers beyond UMass Geosciences. Topics may vary by student interest and can include, scientific and professional ethics of geosciences research, networking, resolving conflict, preparing proposals, non-technical skills, job applications.

Results of new research by students, faculty, and visitors.

Earth surface processes and their relation to topography and landscape evolution. Focus on hillslope, fluvial, and other processes that shape the Earth's surface.

Modern Earth and environmental scientists deal with complex and often very large quantitative data sets that are typically not useful or understandable in raw form. Thus, quantitative data analysis skills are highly desired and useful in quantitative Earth science subdisciplines. This course provides an introduction to processing, visualizing, and interpreting quantitative Earth and environmental science data using scientific computing techniques widely used in the Earth sciences. Computational methods and visualization will be performed using the scientific computing language, python.

This is not available at this time

The field of Hydrology has long separated the study of surface water (streams, lakes, etc.) from groundwater, despite the clear connection of these systems. Over the last two decades, surface water and groundwater have increasingly been viewed as a single resource, producing a myriad of new and exciting scientific work on the subject. The quantity and quality of surface water can affect the volume and chemistry of groundwater, and vice versa.

Not available at this time.