Introduction

Thank you for your interest in our program here at Lehigh University. The Department of Earth and Environmental Sciences (EES) has 14 full-time faculty that cover a broad range of disciplines in Geology, Ecology, and Environmental Science. I am a fluvial and tectonic geomorphologist specifically interested in the long-term evolution of landscapes, the fluvial response to active tectonics, and watershed response to human-dimension climatic change. EES has active research programs in all of these areas and we are aggressively recruiting outstanding graduate students to build the graduate program in these and related disciplines. The faculty I collaborate and interact with most closely here are Peter Zeitler (tectonics and geochronology), Ed Evenson (glacial geology and geomorphology), Anne Meltzer (seismology, geophysics), and David Anastasio (structural geology). I've got a new collaboration underway with our ecologists and environmental biologists (Don Morris, Craig Williamson, and Bruce Hargreaves) working on the ecology and physical hydrology of the Lehigh River watershed.   And I maintain close research ties to Les McFadden, Karl Karlstrom, and Jane Selverstone at the University of New Mexico (my former institution), as well as to Mark Brandon at Yale University.

Research in surficial processes is well represented across the board in EES. It is one of the few Departments nationwide with two geomorphologists of complimentary expertise on staff (Pazzaglia and Evenson); Peter Zeitler and Bruce Idelman (research staff) have brought a new He/U-Th thermochronology lab on line dedicated to understanding near-term exhumation of orogens; the ecology group has a long standing excellent reputation for expertise in limnology (Heargreaves and Morris) and paleoecology (Yu) and our geochemist (Peters) has an active research programs in watershed-scale aqueous geochemistry. Our commitment to excellence in surficial processes is complimented by our recent hires of a soil geologist/ecologist and paleoecologist.

OK, OK!!!  This is not the view from the University (wish it was).  But this place is real close by!  It is the view looking northwest at the five water gaps at Harrisburg - perhaps the one, most important place where Davis and company struggled to understand the origin of transverse drainages.  Lehigh University is actually located on the northern flank of Pennsylvania’s Blue Ridge (South Mountain) and has a commanding view of the Lehigh Valley (Great Valley) and Ridge and Valley of the Appalachians to the northwest. This is the landscape of Davis and Hack. It is where the great geomorphic discourses on long-term landscape evolution were born and continue to be lively debated. Far from a "dead" orogen, the Appalachians have a complicated post orogenic exhumational history and stand as one of the best studied orogens in the decay stage of its evolution. These studies, some of which are now ongoing funded research projects in the EES Department, are investigating the causes of late stage rock-uplift and exhumation through the relatively new technique of He/U-Th thermochronology. Over a distance of only 250 km, one can travel from the subsided Tr-J rift-flank uplift buried under a wedge of Coastal Plain sediments, across the Fall Zone, a flexurally-maintained hinge of the isostatically-rising continent and subsiding Coastal Plain, through the high grade metamorphic heart of the formerly Andean-scale late Paleozoic Appalachians on the Piedmont, to a continental rift basin formed during a time when the area around Lehigh looked like the Basin and Range, into the Ridge and Valley, the fold and trust belt of the late Paleozoic Appalachians, and finally, the Allegheny Plateau, the seaward facing escarpment marking the present-day location of the drainage divide in its slow, but methodical westward march.

In addition to the exciting orogen-scale tectonic geomorphology research in the Appalachians, the setting is well suited to studying climatic, ground water, and coastal processes. A wide range of glacial and periglacial deposits in central and eastern Pennsylvania preserve a rich record of the effects of past climate changes on landscapes. Ground water geomorphology is well-expressed in the numerous karst systems underlying Pennsylvania’s carbonate valleys. And easy access to beaches on the Atlantic coast provide a hands-on experiences of coastal processes and change.

The research and graduate program for geomorphology students is decidedly field-intensive and designed to afford opportunities to learn about the geomorphology in Lehigh’s own backyard, as well as the individual's location of study. Current research is motivated by three primary interests:

• Long-term landscape evolution at the orogen scale and the dynamic feedbacks between the deep earth processes which act to uplift rocks and the surficial processes which act to exhume rocks.
• The processes responsible for the formation and preservation of fluvial terraces and the reconstruction of high-resolution fluvial stratigraphic records through the use of soil geomorphology, numeric age dating, palynology, and cosmogenic profile dating.
• Documenting the effects of past climate changes on the landscape and understanding those changes in the context of human-dimension effects of global climate change on watersheds.

• Observation, organization, and correct geologic interpretation of geomorphologic field-based data. This will include, for many projects, the completion of a detailed geologic map.
• Quantification of the landscape and watersheds through the acquisition, manipulation, and application of digital elevation models. This will include, for many projects, a firm understanding of GIS and several GIS software packages.
• Understanding of the pertinent geomorphologic processes in their study in quantitative terms. This may include for some studies, the construction of a physically-based numeric model and/or flume-based models.
• Effective writing and communication of the subject matter as published papers. M.S. students will be guided in the process of preparing a single manuscript that will also serve as their M.S. thesis. Ph.D. students should be prepared to submit three manuscripts, the integrated sum of which will constitute the dissertation.

Current geomorphologic and related research projects include the studies of two M.S. and one Ph.D. student.

Karl Wegmann is a fourth year Ph.D. student broadly interested in active tectonics and tectonic geomorphology.  Karl is working on active tectonic problems in Italy and Crete.  He is an expert in mapping and dating river and marine terraces and uses these data extensively in his research.  Karl has very broad geographic as discipline interests.  He has worked on everything from Quaternary paleoclimate to paleoelevation in Mongolia.  Karl has written NSF and GSA grants to help fund his research.

Luke Wilson is a second year M.S. student that I am sharing with David Anastasio.  Luke is working in northern Italy on the Salsomaggiore anticline, near the city of Parma.  Luke is taking advantage of exposures in strike normal rivers and the terraces of those rivers to reconstruct the growth of this anticline.  He is interested in linking the anticline growth to the overall dynamics of the collision that is driving the uplift of the Apennines and subsidence of the Po foreland.  Luke is a real expert in GIS and related computational methods.  He has written AAPG, NSF, and GSA grants to help fund his research.

Matt Bennett is a second year M.S. student interested in fluvial geomorphology.  Matt is working on channel dynamics and legacy sediments in the Saucon Creek watershed.  He is balancing his field work against analogue flume models where he is looking at the sediment transport rate as a function of sediment supply and fluctuating discharge.  Matt is really handy at instrumenting watersheds and in the computational analysis of field data.  His research is being funded by the State of Pennsylvania, DCNR and DEP.
   

Current, pending, and just some ideas for research projects in addition to those associated with the above students include:

• Appalachian geomorphology and U-Th/He thermochronology FUNDED (03/01/00-02/31/03)
• The causes of tectonic extension and collapse in a contraction orogen: The northern Apennines (NSF, with Mark Brandon, Darrel Cowan,  Sean Willett, Darryl Granger, Peter Reiners, and a host of Italian collaborators) FUNDED (09/01/02-07/31/07).
• Active tectonics of Calabria (with Paola Molin and Francesco Dramis).
• Long term drainage evolution in Italy (with Walter Alvarez and Mauro Coltorti).
• The Quaternary record of drainage basin erosion in the Appalachians (NSF, collaborator with Paul Bierman and Ari Matmon)
• Fluvial record of incision in a mature, uplifted forearc high, Olympic Mountains of western Washington (NSF, with mark Brandon, Eric McDonald and John Gosse)
• Testing the stream power law using rising anticlines (with Mark Brandon).
• Record of mid-Holocene neoglacial events in the Sangre de Cristo Mountains, Colorado preserved in the terraces of the Huerfano River (with Grant Meyer).
• Geomorphic and ecologic characterization of watersheds in the Pocono Mountains, Pennsylvania; what controls the penetration of UV in streams and rivers (with Don Morris, Craig Williamson) FUNDED (08/01/02-07/31/05).
• Flume studies designed to investigate, among other things, the initiation and evolution of knickpoints.
• Active Tectonics and geomorphology in Ecuador (with the Lehigh Tectonics Group)
• Interactions between rising anticlines and rivers, an integrated geomorphological, seismological, and structural geology perspective (with Anne Meltzer, Dave Anastasio, and Martha Cary Eppes).
• The location of continental divides, base level fall, and exhumation of the Rockies (with Joel Pederson).
• Active tectonics in Crete (NSF-Pending)
• Landscape evolution in the Rocky Mountains - the relationship of the sub-summit surface with Green River basin deposits.
• TCN, grain size, and hillslope processes FUNDED (SGER - 06/01/07-05/31/08).

A reasonable measure of what prospective students might expect out of a graduate degree from Pazzaglia's program at Lehigh is to know what former students are now doing.  Keeping in mind that these folks have driven their own success, here's a list of the current activities of former students where I was the major advisor (in the order of their graduation):

Antonio Garcia (M.S.; PhD USCB)                                      Associate Professor - Dept of Physics, Cal Poly State University (San Luis Obispo)
Merri Lisa Formento-Trigilio (M.S; PhD Penn State)          Exxon/Mobile Research and Development - Houston
Dan Koning (M.S.)                                                                 Employed by New Mexico Bureau of Mines and Mineral Resources.
Karl Wegmann (M.S.)                                                            Employed by State of Washington Department of Natural Resources;
                                                                                                now continuing his PhD studies at Lehigh.
Paul Wisniewski (M.S.)                                                          Environmental Consulting firm - Hawaii.
David Mitchell (M.S.)                                                              Employed by private environmental consultant, Washington State.
Justin Pearce (M.S.)                                                              Employed by William Lettis and Associates, Oakland California
Sarah Newland (M.S.)                                                            Employed by SFEI, San Francisco California
Joel Pederson (Ph.D.)                                                           Associate Professor - Utah State University.
Kurt Frankel (M.S.) (PhD USC)                                            Assistant Professor - Dept of Earth and Atmospheric Science, Georgia Tech University.
Patrick Belmont (Ph.D.)                                                         Post-Doc, NCED, University of Minnesota.
Josh Galster (Ph.D.)                                                             Assistant Professor - Dept of Earth and Environmental Science, Montclair State University

The graduate student in geomorphology can expected to take a wide range of course offerings in EES as well as supporting related sciences from other Departments, particularly Civil Engineering. Specific course offerings (400-level are graduate courses) in any two year teaching cycle may include (* = core course):

• EES 316 Hydrogeology
• EES 319 GIS and computation analyses in geomorphology
• EES 341 Field geology (field camp)
• EES 351 Limnology
• EES 373 Environmental thermodynamics
• EES 384 Lake ecosystems (field camp)
• EES 407 Seismology
• EES 412 Advanced Fluvial and Tectonic Geomorphology
• EES 414 Glacial and Quaternary geology
• EES 415 Paleoclimatology *
• EES 418 Advanced Quaternary geology
• EES 419 Advanced topics in fluvial and tectonic geomorphology
• EES 426 Tectonic processes *
• EES 427 Orogenic belts
• EES 458 Reconstructing Environmental Change
• EES 484 Aquatic ecosystems *
• CE 320 Flood hydrology and hydraulics
• CE 321 Open channel hydraulics
• CE 345 Geo-Environmental engineering
• CE 424 Surface water hydrology
• CE 425 Hydraulics of sediment transport
• CE 456 Behavior and design of earthquake resistant structures

For more information, please feel free to contact the Department of Earth and Environmental Sciences. You can fill out and submit an application via the web by following this link. Also, please feel free to email or call Frank Pazzaglia at (610) 758-3667.