Department of Geophysical Sciences

 
 

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The Department of Geophysical Sciences teaches courses in geography, geology and physics. Students benefit immeasurably when department-sponsored field trips allow them to see the things they have studied in the classroom. The GeoClub  helps organize student field trips. For distant destinations, students still benefit when their professors have seen the things they teach about. Here are some of the experiences I can bring to the classroom. 
 

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Winter (the best season)

Here is a picture of the Guth homestead in  Copper Harbor , Michigan. When we built the house in 1970, we used the tree line to indicate how far damaging waves crashed onshore and therefore how close we could safely position the building. Trees, with their long life spans, can record growing conditions over 10's or 100's of years. The same idea allowed Köppen to classify and map the world's climates using the sparse climatological data of the late 19th century.     

Erosion is not a problem here. The shoreline is composed of the Copper Harbor conglomerate that has been around for 1.8 Ga (billion years). The lake level is controlled within a metre by the locks at the Soo, so rising water levels are not a problem either.

Ice formations change daily throughout the winter. These pressure ridges could be gone within 24 hours with a wind shift over the open waters of Lake Superior. I have seen ice analogues of all plate tectonic boundaries and accretionary prisms develop before my eyes. The house is in the upper right corner. 
 

Summer (too crowded) 

Sunrise over Copper Harbor. The point of light in the center of the picture is the Copper Harbor Lighthouse built in 1866. The Guth homestead is located at the far right of the photo on the Lake Superior side of the point.
Sunset looking west from the house. With a clear horizon and a northern location, the seasonal shift in the sun's position was obvious. Here the sun is setting well over the water. By the time the setting sun touched the furthest point, it was time to go back to school. I got my BS in Geological Engineering from  Michigan Technological University  about 80 km south of here.
Evening thunderstorms over Lake Superior in a view looking due north from the house. When the waters are calm in the summer, a land breeze develops in the evening as the land cools faster than the water. The convergence of the land breezes over Lake Superior provides the atmospheric lift needed to spawn the thunderstorms. 
 

Yooper Links

A Yooper is someone who calls Michigan's Upper Peninsula (UP) home [a UP-er, get it?]. I am only a transplanted Yooper, growing up as a Troll (someone who lives below the  Mackinac Bridge  in Michigan's Lower Peninsula) in Dearborn, Michigan. Yoopers are a diverse lot. Links to the lot:

ISLA DE MARGARITA, VENEZUELA

In 1984 and in 1986, I spent 2 months each year on  Isla de Margarita (11°N 64°N), Venezuela doing field work toward my Ph.D. at  Rice University . The dissertation reference is

Guth, L. R., 1991, Kinematic analysis of the deformational structures on Eastern Isla de Margarita, Venezuela  [Ph.D. thesis]: Houston, Rice University, 582 p.

I only spent two months at a time because 60 days was the length of the tourist visa, and we didn't want to mess with the paper work involved in getting some special visa allowing a longer stay. Except for one week each year, I was there by myself. Unfortunately, any linguistic ability I might have had was destroyed by the 1960's experiment to see if a foreign language could be learned by forcing a classroom full of kids to watch a half-hour TV lesson twice a week. It can't. It is really difficult to explain in broken Spanish to the justifiably curious local people that you are measuring the dip and dip direction of a fault which has not been active since the terrane cooled below metamorphic conditions so they don't have to worry about earthquakes along that fault. It's hard enough to do that in English.
 
View along the eastern shoreline of Isla de Margarita from Laguna de Gasparico. The mountain in the foreground is Cerro Matasiete and the peak in the background is Cerro Guayamurí.
The other side of Cerro Guayamurí from Puerto Fermín. Although composed of igneous rocks and despite its morphology, it is not a volcano.  Serpentinite, an altered slice of the upper mantle, is thrust over the Matasiete Trondhjemite, a granitic body that has a volcanic arc trace element signature. 
Isla de Margarita is a desert island. The sparse vegetation makes the geology relatively well exposed, especially along the shoreline. On the flip side, every plant has spines, thorns, or some other structure used to impale structural geologists looking at the rocks. This site is on the western coast of Paraguachoa between Punta María Libre and Punta Tacuantar.
La roca de El Angel is found on the southern shore of Paraguachoa at Punta Moreno. This natural apparition is composed of a conglomeratic unit in the Eocene turbidites making up the Pampatar Formation.    

Further west, the Punta Carnero Formation is the distal facies of these Eocene turbidites. World class  windsurfing is found near their exposures around El Yaque. 

The local restaurant where I ate each evening. It was then located on the docks in Pampatar. My favorite dish was filete de pargo Pampatar, grilled red snapper covered in a cheese sauce with squid and octopus and then thrown under the broiler for a crusty top. I have yet to back engineer the recipe.
 

DEATH VALLEY, CA

Nine months after finishing by Ph.D., I was still doing mineral separations for Ar/Ar age dating on samples from Isla de Margarita. The final hand picking is very tedious, examining each sand-sized grain and removing any grain that is not a pure grain of the desired mineral. Measure out about 500 mg of sand to get an idea of the sample size needed to be examined grain-by-grain. So, when  Laura Serpa  and  Terry Pavlis  (friends from  University of Utah  now teaching at  University of New Orleans - UNO ) asked me to spend March 1992 driving visiting scientists around   Death Valley , I jumped at the break. The visiting scientists turned out to be a Russian geologist and Ukrainian geophysicist who spoke little English. Since the Soviet Union officially broke up 26 December 1991, just two months earlier, they were anxious for news from home. When you don't know Russian, nothing can prepare you when you have to act as "translator" for two former Soviets trying to buy a short wave radio from a very patient Circuit City salesman. To further complicate the negotiations, we had to get adapters so the radio would also work using the 220 V, 50 Hz power supply in Russia.
 
Dantes View: The high point in the upper left corner is Telescope Peak, with an elevation of 3368 metres. The valley floor is 86 metres below sea level. The two points are only 23 km apart, making this topographic relief one of the greatest in the US. Vladimir "Volodija" Shevchenko, Cindy Fallgatter (the local grandmother carpenter), and Alik A. Lukk at the Pfizer base camp in Shoshone, CA. The camp is now the  Shoshone Education and Research Center , available for student groups through Terry Pavlis at the University of New Orleans. 
 
Volodija and Alik had been with the UNO crew for some time before I arrived. By the time the UNO crew left 5 days after I arrived, Volodija and Alik were tired of the American cuisine. They asked if I would mind eating the food they were accustomed to and I told them that  I was a field geologist. That was sufficient to convince them that I would be happy with anything. Lots of fried or boiled chicken with rice or macaroni or corn flakes for breakfast, soups or potatoes and cabbage for evening meals.  Recipes for the field are generally more varied for American students.

Alik flew home. I drove Volodija back to Houston from Death Valley. To reduce meal expenses, Volodija filled a cooler with bags of boiled chicken, boiled potatoes, macaroni and cole slaw. Bread, corn flakes, cheese, deviled ham and milk rounded out the provisions for the road trip. The only other things we needed were a full tank of gas and, the way the Ford Ranger kept stalling out, a stiff tail wind.
On our four-day road trip from Death Valley to Houston, we stopped at  Zion National ParkBryce Canyon National Park (shown above), and  Carlsbad Caverns National Park . Volodija Shevchenko examines the dead Ford Ranger at  Monument Valley Navajo Tribal Park . The black box that substitutes for a distributor had to be replaced. This car repair was one of the high points of the trip for Volodija. Apparently in Russia, the driver brings tools and repair parts to fix his vehicle in the field. Here with just a credit card and AAA membership, we were on our way again in about three hours .
 
 

RESORT GEOLOGY

French Polynesia

Flying into Bora Bora. The barrier reef and enclosed lagoon are clearly marked by the color of the water. Flying into Bora Bora. The extinct volcano that forms Bora Bora has been dissected by erosion. Geologists interested in understanding the internal structures of volcanos are condemned to work in places like this.
 
 
Bora Bora by boat.  Another fast sunset. At about 18°S latitude, the twilights were much shorter than what we were used to in the summer at Copper Harbor with its latitude of about 47.5°N. I will always find it remarkable how the Polynesians could  navigate  the vast South Pacific and hit these tiny specks of land, guided only by the stars and the swells.
 

St. Kitts-Nevis 

St. Kitts and Nevis are part of the Lesser Antilles island arc, where the Atlantic lithosphere is subducted beneath the Caribbean plate. Island arc volcanism typically produces a viscous magma that creates the steep slopes of a composite volcano (aka stratovolcano) as shown above. Many sugar plantations have been converted into inns. Do you what to learn more? Take  Caribbean Cultures (IDIS 2400 in your catalog). An optional seminar visits St. Kitts and Nevis over winter break. 
 
 

Baja California, Mexico

  Over the semester break during the 1986-1987 academic year,   Laura Serpa  and  Terry Pavlis  (friends from  University of Utah  now teaching at  University of New Orleans - UNO ) asked us to join their UNO student field trip through Mexico. They could only get one departmental van and we could supply a second van and a relative who speaks fluent Spanish. It was a win-win situation for everybody. We drove down Baja California to the ferry landing near La Paz. An evening ferry trip across the Gulf of California put us into Los Mochis where we caught the train through the Parque Nacional Barranca Del Cobre to Chihuahua. From their, we drove through Presidio and Marfa, TX ( no lights seen ) and back to Houston or New Orleans.
A Boojum Tree "forest" in Baja California.    

But oh, beamish nephew, beware of the day    
   If your Snark be a Boojum! For then    
You will softly and suddenly vanish away,    
   And never be met with again!    

But if ever I meet with a Boojum, that day,    
   In a moment (of this I am sure),    
I shall softly and suddenly vanish away--    
   And the notion I cannot endure!    

In the midst of the word he was trying to say,    
   In the midst of his laughter and glee,    
He had softly and suddenly vanished away--    
   For the Snark was a Boojum, you see.    
    

Rev. Charles Lutwidge Dodgson
The Hunting of the Snark, 1876
The UNO departmental van is being loaded in a boxcar for the train trip through Copper Canyon (Parque Nacional Barranca Del Cobre). Our van is on deck. In situations like this, you are glad you bought that Mexico car insurance at the border. Unlike the state-sponsored collusion found in Massachusetts, Texas and most every other state in the union uses a free market to set auto insurance rates and coverage. Even so, our normal policy would not cover damage to the van while riding in a Mexican boxcar.
 Copper Canyon in Mexico is often compared to the Grand Canyon visited by the GeoClub in  1998 . The morphologies are quite different due to the differences in geology and climate.
 
 

OTHER PLACES

In the summer of 1977, I worked for  Exxon  as a field geologist. We alternated one week in the office in New Orleans with one week in the field along a West Virginia seismic line. Surface control was needed to interpret the seismic data.
I lived in Utah from 1977 to 1981 while I worked on an MS in Geological Engineering at the  University of Utah  in Salt Lake City. This is Delicate Arch in  Arches National Park .
Salt Lake City, Utah is located in a valley susceptible to temperature inversions that trap in air pollution. The state capitol dome is in the lower right corner. From that vantage point, state leaders can see smoke from the 370 metre-high smelter stacks across the valley in Magna, Utah hit the inversion layer and spread out horizontally. It is a  rare thing when the public price of corporate appeasement escapes the smoke-filled back rooms under the capitol dome and is made manifest for all.
In the summer of 1978, I worked as a field hydrologist for the  Water Resources Division  of the  US Geological Survey . I was supposed to collect water quality data from springs and seeps on National Forest land in the Wasatch Plateau of central Utah. As shown, much of the plateau is near timber line. All National Forest land is open for multiple uses, and base-line water quality data were needed in case the area was opened up for coal mining.    

On Mondays, I would check out this Jeep CJ-7 from the General Services Administration (GSA).  By Wednesday, I'd have blown a head gasket which routed the blue exhaust up the steering column. Old timers finally told me they took their own tools in the field and would retorque the head bolts before they bedded down for the night. Sleeping next to a hot exhaust system is almost as good as a dog.

Joes Valley Reservoir in the Wasatch Plateau. As you might have guessed from the straight cliffs on the far side of the reservoir, the dam was built along the strike of  Joes Valley fault . It is therefore considered a  high-hazard dam by the state of Utah. (It's the dot in Emery Co. below the "E" of  "SANPETE".) You might want to think twice about taking that corporate transfer to Orangeville or Castle Dale, Utah -- the towns located downstream of this dam.
Leaving Utah to join my wife in the swamps of Louisiana was a shock. We spent a year in Lafayette, LA working for  Conoco  as geophysicists. This is the Atchafalaya just east of Lafayette.     

Cajun country had great food, great people, great music, but a rotten climate. We can get some food by mail from  Konriko Rice Mill or  Zatarain'sBoudin is harder to get.

After a six-month research and seismic processing stint in  Ponca City  OK, Conoco told us they just had one job for the both of us. Wisely, they kept the person having some hope of fitting into the Big-Oil  corporate mold and transferred her to Houston. I started my Ph.D. in Houston at  Rice University   

Unlike Salt Lake City, Houston, TX (shown at the left) is one of those cities built on the coastal plain with no physical barriers to urban sprawl. Houston has done this in typical Texas style -- BIG. A big city with a miserable climate and a "Wonder-Bread" culture has no redeeming features.

Conoco transferred my wife and family from Houston to Corpus Christi in 1987 and then back to Houston in 1991. The corporate line is that frequent transfers gives employees varied experiences. In reality, it is done to destroy family and community ties so that The Corp. becomes mother and father ( you thought J. Michael Straczynski could just dream up the Psi Corps? ).    

In Corpus Christi, we lived just across the bridge from  Padre Island National Seashore . Our house was across the street from the Naval Air Station where the  Blue Angels  performed each year. The house backed up on a pond created from the borrow pit used for fill in building the air station, and the pilots used the pond as a target to line up their maneuvers. As a result, they flew right over our roof (at left).     

In 1992, Conoco told my wife to transfer back to Lafayette or be down sized out of a job. Looking at the 5th transfer in 10 years, we went  home.

 
   

Page and photos by Guth © 1998.08.19
last updated 2000.07.12