Mandeville |
UNO & Yucatan |
David |
Innsbruch |
Divorce |
Cellie's Death |
Yucatan Hydrology & Geochemistry |
Marriage |
Life has its pivotial moments for each of us. And the move to Mandeville and UNO was a major one for me. The department had 11 full-time faculty members and the next 23 years was the highpoint for the department. I could not forsee the future and know that budget cuts following Hurricane Katrina, Republican state politics, and the relentless opposition of LSU to its existence would reduce UNO to the shell that it is now in 2017. But this was 1982 and I was 35 years old, an Assistant Professor in a tenure track position. At the university, I could no longer pretend to be a graduate student mixing in with the students, living the good life. I had to decide how much time to devote to research and teaching and how much time to devote to life's other responsibilities. I had accumulated various pieces of scientific equipment, including titanium reaction vessels built by Bill Seyfried with a grant from Clyde Moore's research group at LSU. And I moved them to UNO during the summer, setting them up in what had been Gary Allen's Geochemistry Labratory, the UNO metamorphic petrologist who was not doing research. But most important, we needed to find a house to live in Mandeville. Meanwhile Louise found a job as a psychologist at nearby Southeast Louisiana Hospital and David was enrolled at the Mandeville Elementary School on Monroe Street.
I asked Cellie to divide these lakefront properties among her three children. The thought of living on the lakefront with its beautiful view of Lake Pontchartrain had always been in the back of my mind. I wanted to refurbish the rental house and use it as our home. But Cellie did not want to lose the rental income. We were discussing this in the driveway of the rental house when Uncle Clay stopped by. Clay supported me, telling Cellie that at her age, she needed to resign herself to relinquishing some control of her properties, especially since I was there to help her. She was not impressed and said "No!" So Clay offered a rental house on Jackson Avenue near the railroad tracks that we could rent while building a house. And we moved there. Over the next few months while checking out available Mandeville lots, Cellie relented and let me have the front third of the empty Lakefront lot, giving Marilyn and Lloyd the swampy back portion. In return I agreed that Lloyd and Marilyn would eventually get the other two Lakefront lots as part of their inheritances. We had sold our Baton Rouge house and would use the proceeds towards building a house. And Cellie loaned us necessary additional money at 8.5% simple interest which was the going rate. Later, I discovered she was banking her friend Dale Gale at 8% interest. I asked her if this was fair to me, her only remaining child in Louisiana. She replied "Dale is a better credit risk." (LOL). Dale Gale was a tough antique dealer who, we use to laugh, would sell you her bed to make a sale. But she was a good friend and, like us, could be trusted to do business with a handshake - not a common trait today. In 1991, after Cellie died, Dale still owed the family a substantial sum of money and there was no legal, written record. And she just wrote out a check to repay the family without me asking.


At the beginning of the 1982 fall semester, Bill Ward and Al Weidie led a geologic field trip to the Yucatan where they had been doing field work (mapping, stratigraphy, and structure) and carbonate petrology studies. The field trip was attended by scientists from all around the country. Bill had done his Ph.D. research (under Robert Folk at UT) along the Yucatan Caribbean coast and was now the recognized authority on its carbonate coastal geology. I developed great respect for Bill Ward and enjoyed working with him. Al had done his Ph.D. research (under Clay Durham at LSU) in northern Mexico and had later joined with Bill to work in the Yucatan, doing structure and stratigraphy. Al's wife Anna came along on the trip, a beautiful Mexican woman (from northeastern Mexico) he had met doing his Ph.D. field work. I can close my eyes and still see Anna standing on the cliffs near the white Mayan ruins at Tulum, looking down on the green Caribbean Sea with her long black hair and dress blowing in the wind. What a beautiful, romantic location to work in. This field trip got me started on a life-long career as a "resort" geochemist. I could recognize a fun place to work when I saw one!
And I wanted to delineate the water movement. In general the fresh-water lense in the rock pores was thin, tapering to zero at the coasts, and overlay seawater in the rock pores which entered near the coasts. The halocline where seawater mixed with overlying freshwater was a zone of dissolution, creating the network of caves. This zone of dissolution moved vertically up when the regional sealevel rose and down when it fell. We knew the freshwater moved from the interior towards the coasts and suspected that the underlying seawater moved under the peninsula between the Caribbean Sea, the Gulf of Campeche, and the Gulf of Mexico. But we didn't know the rates of fluid flow, the specific movements within the two water masses, and how the seawater and freshwater chemistries evolved through water-rock interactions. I wanted to find out what was happening. And the fun part would be scuba diving in the cenotes (sinkholes) and caves for the sampling and water-tracing programs.
I want to start with Jeff's research in 1983 at Xcaret. Back then it was at the end of a dirt road with a chicken farm near the cave entrance by a few Mayan ruins. We were young and Jeff, Woody, and I would race the rental car on that dirt road to see who could drive it in the shortest time. I never won. The mouth of the submarine cave led to a short caleta (a lagoon about a hundred and fifty feet away). Being reckless, we swam the cave with underwater flashlights, without scuba gear, using the air that collected in several places at the cave ceiling. The air layer could be recognized by light reflection and was just thick enough to push a snorkle into it to grab a breath. There was one point in the cave where a ray of light came through from a crack in the roof, and the water refracted it like a prism, leaving a patch of colors on the floor, seemingly marking the location of a non-existant Mayan treasure. The freshwater water flow to the Sea was too strong to swim back to our starting point so it was scary the first time. But it was fun! Within 10 years, Xcaret had been rebuilt into a Mayan Disney World, a tourist trap. In 1992, I swam the underwater cave one last time, only to surface into the lagoon adjacent to a sewage pipe coming down from a new hotel above the cave. Sadly, humans will destroy everything beautiful in nature in their endless quest for personal profits. What a loss for all of us!

An offshore coral reef protected the shore areas and provided protected areas for snorkling. Now in 2017, most of the offshore coral reef and interior patch reefs are bleached, the sea urchins have disappeared, and the active sea turtle support groups that protected their nests have been disbanded. The little beach town of Akumal was a paradise in 1980s and 1990s. Now development and tourism at Akumal Bay has robbed it of much of its charm. Half Moon Bay, north of Akumal Bay and south of Yal Ku Caleta, still retains some of its isolation. The restaurant and bar La Buena Vida still sits on Half Moon Bay and the "Lol Ha" Local Species Bar remains on Akumal Bay. We spent many a late afternoon there with the expatriots watching the sunset and drinking into the night. Resort science is hard to beat as an occupation! These were certainly some of the best times of my life.
On that same trip I wanted to do reconnaissance at Tankah (just north of Tulum) which later became Bruce Ford's field area. Today this area is a tourist resort (Manatee Cenote) but at that time it was known for drug smuggling and there were no roads to Tankah other than a beach trail leading pass an old coconut plantation used to traffic drugs. I had heard there was a cave connecting the Caribbean Sea with a lagoon containing manatees at Tankah. I wanted to check out the area for research and also scuba dive through the cave. Kraig and I drove my rental car south of Tulum and met up with a local drug dealer known for diving in that area. He drove our car into the old plantation area and we stopped at a house with a large table outside, about 15 by 40 feet in dimension. The table was covered in coconuts but there were 10 men standing around it holding assault rifles. Those must have been valuable coconuts! Our driver knew these guys and convinced them (with the appropriate bribes) to let us proceed. The drug dealer drove like crazy on the beach trail, and I remember telling him not to wreck the rental car. He looked at me, laughed and said "No Problemo, Avis!" We all laughed! At Tankah there is a beautiful, winding, long lagoon extending inland, separated from the Caribbean Sea by about a 200 foot long cave that opened under the Caribbean Sea. Locally the lagoon and cave were known for manatees which frequented the area. We swam for awhile in the passageways on the side of the lagoon and then went through the big cave. The water flow was enormous and the cave had numerous conduits, most eventually became too small in diameter to pass through. The danger was that if you picked the wrong passageway, the force of the water flow would prevent your return. The drug dealer knew the way and we followed him. We popped out in shallow water through blow holes in the cave roof 50 feet offshore. This was a great experience. When I came back with Bruce Ford the next year, the drug dealers were gone from the area. I never took a student through the cave; however, we used to pop down into the cave through blowholes off the beach and swim underwater in it to the next blowhole to pop out. Sadly, when I came back one last time on my 70th birthday in 2017, the blowholes were mostly filled in - too dangerous I suppose for the tourists.
With the completion of Bruce Ford's research in 1985, the Yucatan field work went into a hiatus for several years. Amoco, Mobil, Tecaco, and Exxon were supporting my experimental efforts to reproduce oil-field reservoir reactions. I ran closed-system labratory experiments on dedolomitization (to form calcite) and calcite dolomitization. Dolomite and calcite were reacted for 7 weeks under hydrothermal conditions (100, 150, and 200 degrees Celsius and 300 bars), using two of Bill Seyfried's titanium hydrothermal reaction vessels that had come with me from LSU. Lynton Land's former Ph.D. student Dennis Prezbindowski, then in private industry at Tulsa, worked with me, along with Bob Klementidis at EPR, doing the petrology, SEM and electron microprobe work on the reactants and product minerals. We were trying to refine the thermodynamic stability of dolomite, a major geochemical problem due to dolomite's variable ordering and often being nonstoichiometric in composition. The dedolomitization went beautifully but the calcite dolomitization failed due to slow reaction kinetics. The dedolomitization results were published in Geochimica et Cosmochimica Acta in 1987. Running those experiments was like going back in time, being a graduate student again, spending late-night hours doing chemical analyses and monitoring the equipment. The excitement of seeing the SEM photographs of the growing calcite crystals on the dissolving dolomite made all those hours of labratory work worthwhile. Following this work I reopened my sepiolite and kerolite dissolution experiments from Berkeley. The reaction kinetics of silicates is so slow that even now after ten years, equilibrium had to be extrapolated from the final data. The extrapolated sepiolite and kerolite thermodynamic data were published in Geochimica et Cosmochimica Acta in 1988.
I taught alpine geology and physical geology in the Innsbruch summer school twice: the first time in 1986 with Louise and David and the second time in 1991 with David and Londi who later became my second wife. The trips for us started in Wiesloch, south of Heidleberg, at the home of Marilyn, Karl, and their daughter Marcella. Marilyn and Karl had this beautiful home with an empty 3rd floor apartment which we occupied. They had built their house on land leased from the Catholic Church for 99 years. Karl must have been a good Catholic because he certainly knew his communion wine. We would get happily snuckered on their patio in the evenings. I would also get to visit my soulmate Dorothea in Aschaffenburg. From Wiesloch we would do some touring before ending up in Innsbruch. Road trips with me driving were always exciting. I have this scary memory of driving on a single-lane road with David and Louise, falling asleep behind the wheel, waking up quickly, thinking I was on the double-lane autobahn and confused about the slow-pace of cars ahead of us. I switched over to the left lane to pass cars for a mile, driving around a long curve, before pulling back in the right lane. Then a car zipped by heading in the opposite direction in the left lane. There must have been a guardian angel looking after us.
The previous fall, I had met Yolanda (Londi) Harrington Moore, a 31 year old, 5 ft 2, blonde (with eyes of blue) graduate student who had come to UNO to get her M.S. degree. I was 42. Londi was working for my good friend Dale Easley, the UNO geohydrologist. I remember her asking me why should a graduate student take my geochemistry courses. My reply was for knowledge. But, she wanted to know how it would help her in her career. And after telling me I was arrogant, she left my office in a huff. Londi had grown up mostly in Houma in Cajun South Louisiana and had led (I thought) a wild life with two marriages already under her belt. As a teenager, she had been thrown out of one private Catholic high school for doing wheelies on the football practice field and being an accessory to blowing up a school bathroom with dynamite. The latter feat made her a school legend for students coming after her. She later graduated from Centenary College with a BS in Geology while working for a bank and for two independent oil companies. Earlier she had owned and lost a gas station in Brevard, NC. Londi was a Cajun girl to be sure, even though her actual lineage was from a West Texas ranch near the Mexican border (from Yvonne, her Mom) and from North Louisiana (from Jackie, her Dad). We were a perfect match I thought. I had always wanted to date someone with demolition experience. One spring day, I needed a dance partner to finish a Cajun dance course. I had started the course months before with my earlier faculty girlfriend, who had since shown the good sense to dump me. Londi said her major professor Dale Easley told her I was suffering greatly going through my divorce. I agreed, feeling much like the Big Bad Wolf chasing Little Red Riding Hood. She was a breath of fresh air in my life. We would regularly go to the Maple Leaf Bar on Oak Street and end up dancing in the street when it closed. At UNO, I would sometimes wait to catch Londi sashaying down the hall past my office, and reach out to pull her in while closing the door. This intriguing behavior pattern did not go unnoticed, and Dale Easley became somewhat irritated with us. I checked with my department head Bill Craig to make sure our relationship fell within the "normal" guidelines of faculty student affairs (lol). He said not to serve on her M.S. committee or officially teach her any courses. Meanwhile, Londi was sometimes jealous and hence irrational (in my opinion). Once after midnight, she actully poured an ice cold Coors on a very sensitive body part just because I had taken another woman out to dinner. (I had explained to Londi it was a favor to Cellie for a family friend. Women!) This was apparently going to be a long-term relationship.
My two Chinese graduate students (Yong and Yang) and Hattie Brown sat with Londi and me in the front row family pew during the Episcopalian funeral service, to the dismay of my family (LOL). Hattie had been there for us when we were in need. Cellie was buried in that "dreadful" (to me) old Prieto Tomb in Mandeville to be with my father Al, her parents May and Ernest and her siblings Marion and Preston. I don't think anyone else will want to be buried there, and the key to the tomb was subsequently lost by the funeral home. Marilyn and Lloyd had returned for the funeral and even Louise showed up at the wake, not really sure why? It was bitter sweet to see Cellie's old close friends from Crowley: Evelyn Gueno, Beth Barnett, and Margarette Penner and New Orleans cousin Lil Burke. These ladies were not long for this world, and I never saw them again. As I now look into the future, my ending too is not that far off. But at that time, that was not in my thoughts.
I need to step back to being a professor. In the summer of 1989, I was planning a new research program in the Yucatan inland from my previous research area doing groundwater chemistry along the eastern coast. The northern Yucatan surface is fossilized reef rock (limestone) with karst surface, e.g., no surface streams and only cenotes (sinkholes) and wells to draw drinking water from. Rain water dissolves the limestone, sinks downward to the water table, and then flows towards the coast. This fresh water lense is actually brackish with a nearly constant vertical composition and has a maximum thickness of a few hundred feet in the center of the peninsula. Underlying the freshwater lense is seawater moving through rock pores and fractures, between the Caribbean Sea and the Gulf of Campeche. The freshwater is floating on top of the more dense seawater, separated by a narrow mixing zone. Bill Ward had a Mexican geologist friend who was working as a consultant for CALICA, an American subsidary company of Vulcan, located just south of Playa del Carmen. Their property extended more than 10 kilometers inland and they had dredged an ocean harbor to load aggregate to ship to the States and elsewhere. CALICA was mining limestone in open pits (west of the coastal highway) down to the water table, 40 feet below and then dredging more limestone below the water table. Their milling plant on the property would grind up the limestone into piles of aggregate of different sizes, move it by a large conveyer belt to the harbor, and there the aggregate was dropped vertically into cargo hulls of transport ships. By 2000, the pit seemed to be a couple of miles wide. This was really a big operation.
CALICA's operation was impressive with its large harbor (used also by cruise ships visiting Playa del Carmen) and an inland open pit which was a km wide at that time. The mining trucks followed the International Mining Convention of driving on the left side of the road and they were enormous with wheels taller than me. Around the edges of the open pit were drilling rigs, drilling boreholes to set dynamite to enlarge the pit. Hmm - Drilling rigs, those could be useful in my research. Caves were exposed in the pit walls and in later explorations, I found them to be filled with beautiful stalactites and stalagmites. These exposed caves were destroyed in the next series of explosions. Draglines in the pit bottom continuously worked below the water surface to get more limestone, while gigantic trackhoes loaded the trucks with huge blocks of limestone to be taken to be milled into aggregate.
Caves ringed the sides of the cenotes, marking positions of the freshwater/seawater interface when sea level had been higher in the past. Flocks of vultures and other birds were roosting on the exposed edges of the caves while brown vines dropped all the down from the surface to the water. The green water surface had a white sheen over parts of it, marking a floating layer of calcite crystals that precipitated as groundwater degassed carbon dioxide to the air.
Further back in the jungle, several years later, I found a Mayan Cave, (named the Dos Ojos Cave) complete with an altar, tiny rock paths for the "Alux" (the little people of Mayan legend), and Mayan glyphs carved on the wall rock. That cave is so cool! But the jungle was difficult to hike through, even on a path. I never saw a jaguar but did once see a gold-colored big cat (mountain lion?). The ground surface consisted of hard, sharp rock with trees growing out of holes in the rock. Limestone lacks aluminum which is needed to make clays for soil from weathered rock, so there isn't much agriculture in the northern Yucatan. What little soil is present in this area formed from weathering thin layers of volcanic ash, dropped from volcanic eruptions further west in mainland Mexico. The joke was that the Mayans planted their crops in pot holes in the limestone, marking the locations of dead Spanish conquistators which provided organic nutrients for their crops. The surface rock was so irregular that it was easy to fall and cut yourself on the sharp edges. The vegatation seems dangerous such as the Chechen trees which have sap that burns like acid on your skin. Luckily, Chaca tree sap can be used as an antidote, but you have to know your trees. And no matter where I was in the jungle, I was always coming across these ubiquitous, never ending, straight Mayan walls of chunks of piled limestone rock to a height of 2 to 3 feet, presumably built hundreds of years earlier to mark land boundaries. They must have made for life-long jobs of Mayan slave labor to haul loose rock through the jungle to build those walls.
In late summer in 1989 I also made a reconnaissance trip to Barbados to check it out for doing geochemical field work. Ida came along to see the island. Barbados, a former British colony, is much like the Cayman Islands with a very literate African poppulation, religiously dominated by the Anglican Church, and dotted with picturesque tiny, neat, pastel-painted houses. Both consist of a wedge of sediment capped by limestone reef rock. The difference being Barbados sits over a subduction zone east of the volcanic Windward Islands in the Atlantic, rather than along a left-lateral transform fault marking the boundary between the Caribbean Sea and the Gulf of Mexico. I began my trip by meeting government officials in Bridgetown. They did not object to my groundwater sampling program and pointed out the general locations of boreholes along the eastern coast. So we rented a 2 door Jimny Jeep and off we went. The coast was incredibly rugged and beautiful, with steep limestone clifts that had wave-cut platforms marking periods of higher sealevel. There were Caucasians among the Africans, descendants of the original British settlers, that I made friends with. In general, they seemed to have gone to New Zealand and Australia to find mates. So that was how they maintained a somewhat distinct ethnic group but everyone seemed to be (at least) distantly related. Although I added the Barbados groundwater chemistry to my data base, this trip and others later were more for fun than science. After all, I needed to maintain my growing reputation as a "resort" geochemist!
The trip itself was an experience not to be forgotten. On the drive down from Cancun, the rental car's transmission broke down on the narrow two lane coastal highway. The car was off the road and partially in the jungle. I told everyone to hide in the jungle while I hitchhiked back to Playa del Carmen to get another car. Well Londi was excited and climbed up on top of the car and started dancing. Sometimes a girl just has to dance! About this time a deuce and a half truck, the back filled with Mexican laborers, whizzes by. The truck came to a screeching halt and then started backing up to the broken-down car while the Mexicans waved machetes and cheered Londi. Her Spanish was and is still terrible, and she frantically waved to them not to come to her aid. They were very disappointed. Yong and Yang then pulled her off the car, wrapped her in a blanket and hid her in the jungle until I got back. Those boys knew how to handle a woman! At Akumal, we rented a condo on Half Moon Bay. The first afternoon, Londi and I went snorkling, collected conchs and laid them out to dry. The next morning we woke up to the smell of fried conch. Yong and Yang had scooped out the critters (mollusks) and were cooking them for breakfast (lol). Luckily, they didn't know how to recognize where the sea turtles had buried their eggs in the sand or there would have also been a sea turtle egg omelet. We later went to nearby Xel Ha, a tourist lagoon with thousands of colorful tropical fish. I had to save the fish from Yong and Yang. They looked at them and said "Chinese Takeout! Let's grab a few." They were great fun to be with. In the evening after doing field work, we would drive to Playa del Carmen for dinner and drink "grande" margaritas until we were drunk as skunks. What a week that was. On returning to New Orleans, immigration officers detained Yong and Yang for several hours. The officers would not tell me why, and I refused to leave without them. Eventually they were released without me being arrested for insulting immigration officers - a minor miracle for me in dealing with the government.
The August, 1990 field work in the Yucatan had gone well. The boreholes were waiting for us at CALICA and John Clark assigned two employees Jorge Rodriguez Bremauntz and Lourdes Rodriguez to help us. Both became close friends as well as Marie Carmen Cerda, the secretary who took us under her wing. We ran depth vs conductivity (also pH, temperature, and dissolved oxygen) profiles in the boreholes and in the cenotes to define the geometry of the freshwater lense at each location. The freshwater lense was 10 to 15 meters thick, brackish with a constant composition, and it had a sharp interface with the underlying seawater. As expected it decrased in width approaching the coast. Yong and Yang took groundwater samples in the boreholes and I did the same in the cenotes. We measured all the chemical components in the field that would change before we got back to UNO, e.g., hydrogen sulfide. And Londi did field tests to measure the rate of groundwater flow across the boreholes. We would insert a pipe in the borehole from which hung a conductivity probe and a tube to inject seawater (in the freshwater zone) and fresh water (in the seawater zone) and then subsequently record changes in conductivity with time to estimate the groundwater velocity. I thought the field data we took was really good. Londi and I came back in November, 1990, to remeasure the geometry of the freshwater lense to see if it was changing seasonally. The changes were insignificant. The freshwater lense in the Yucatan is much thinner than would be expected for a static system because it is dynamic with the water flowing coastward. The yet to-be-explained features were the uniform brackish composition of the freshwater lense and a temperature spike in the halocline below the lense. Those explanations would come later.
During the 1990 Yucatan trips, Londi and I met James (Jim) Coke one evening at the "Lol Ha" bar on Akumal Bay. Jim was an expatriate from Texas, a cave diver who had become a scuba diving legend for mapping underwater cave systems in the Yucatan, a very dangerous profession. Jim was built like a field geologist, thin as a reed, all muscles, with an unmatched capacity for alcohol. He had read my earlier paper on the groundwater chemistry along the Caribbean coast and was interested in our research. A biologist by training, Jim discovered an 11,000 year old skeleton in a local submarine cave system and published his find in Nature. At the time, I think it was the earliest human dated in the Americas. We later worked and published together. Jim knew the jungle locations of the cenotes, acting as my guide, and took me scuba diving into submarine caves. On my last Yucatan field season in 2004, we drove across the peninsula, sampling the deepest cenotes in the Yucatan. He was a wonderful friend, not to mention a good drinking buddy at La Buena Vida on Half Moon Bay. I remember him always greeting Mayans in the field by calling them "jefe" (boss). I eventually lost track of Jim and was told by the Akumal Dive Shop owner in 2017 that Jim died in 2016. Than in 2019, like Christ, Jim resurrected (resurfaced). I hope to see him again.
The picture shows Londi at a cenote named Car Wash, about 5 km inland on the road to Coba. I remember diving into the water and at the height of my dive, a local Mayan yelled "Cocodrilo!" (crocodile). But he was a small 4 ft freshwater cayman, nothing to worry about (lol). Our big event in 1991 was for me teaching UNO summer school in Innsbruch, and I took Londi and David with me. As in previous trips, we flew in to Frankfort, went to Wiesloch to see Marilyn and Karl, and did a side trip to Aschaffenburg to see Dorothea. I do remember driving in France with Londi and David and nearly getting us killed. There was a road intersection with a road coming in from the right. We were going straight and I erroneously assumed we had the right-of-way. An 18 Wheeler turned in front of us and we went careening out of his way. Londi said "OK, you have good reflexes. Don't do it again!" Londi and I visited Chamonix near Mt Blanc on the trip to Innsbruch. The French Alps are so beautiful. We drove up high in the mountains and joined a crowd watching two person parargliders jump off the mountain edge and glide away in an updraft. One pair ran up to the edge, jumped, and dropped like a rock out of sight. But no one seemed worried about them. Hmm, could this be natural selection for paragliders. Pairs continue to jump and glide away. Then, twenty minutes later, two pairs of hands appeared as a couple pulled themselves up over the edge of the mountain with their paraglider. Wow, those were tough people. Londi thought Charmonix was the most romantic place she had ever been. I made the same mistake that I had made with Louise in Mombasa. I promised Londi we would come back in 5 years and we never made it back. Never promise (your wife or future wife) something and not deliver.
In Innsbruch, we rented an apartment on the other side of the Inn River on a very steep hillside. Earlier that year (in May) when Londi and I went back to CALICA for a week of fieldwork, our Mexican field guide Jorge mentioned he was going to Europe that summer. We had invited him to visit us. At the beginning of the semester, Jorge flew in to Munich and I went to pick him up. I brought him back to Innsbruch where he stayed with us for a week. The Austrian border police detained him at the border overnight because he had come from Mexico. I saw firsthand the prejudice of nationalities. The first day Jorge rented a bicycle and said I'll be back that evening. About an hour later, he appeared at the apartment, all bloody and carrying the bicycle, totally smashed from a crash. That was a very steep road! But after nursing him back to health, we had a good time and were sad to see him leave, as were the Austrian girls. That is probably why the Austrian border police didn't want to let him into Austria - to protect the virtue of their Frauleins - an unsuccessful mission. Jorge never went back to Mexico permanently but stayed in Europe and married an Italian girl.
But it was a great time for the students and us. Londi soon became their earth mother, their mother away from home. And David made friends and partied with them. They would ply him with alcohol in the hope of getting advance copies of my tests. Not a chance! He was still largely uncontrollable (in my mind) and was being sent to an Outward Bound Camp later that summer to shape up! He and Londi came on the field trips with us looking at glacier-carved features and rode ski lifts to the tops of mountains to examine the glaciers. Near the end of the term, David and I did a recon trip to a glacier in the Italian Alps where the students were going the next week to collect red garnets that had weatherred out of the clifts above the glacier and fallen on top of the ice. To get to the glacier, we had to hike for a mile on a path over a steep end moraine, after getting off a ski lift. We overtook an elderly British couple who must have been retired university professors because they were closely examining the flora. I stopped and asked the lady if she could identify a flower near the path. She said "Oh, Let me look." and bent down. Suddenly, she slipped and went rolling down the hill, crashing into a boulder. Her husband and I ran down. "Are you hurt?" he cried out. She looked up and held up her hand which was bent 90 degrees backwards. "Oh, I'm fine but I do believe my wrist is broken!" she replied. "Not to worry my Dear. Have some of this whiskey." and he poured her a shot from a flask which she sipped on. I was amazed. She didn't cry or complain and must have been in terrible pain. I guess that is what the British call having "a stiff upper lip." Meanwhile, I retreated rapidly, feeling partially responsible for her fall.
The summer went by quickly. Londi was disheartened that the Austrians didn't celebrate the 4th of July with a barbecue (unpatriotic heathens). We took a weekend trip to Vienna, one to the Dolomites in morthern Italy, and one to Venice and to various local sites. The trip to Vienna followed the Danube River and what touched my soul were the stone ruins of a small castle (Durnstein Castle) where King Richard the Lion Heart had been imprisoned for ransom when returning home from the Crusades. We were there alone (no tourists) at dusk and I could easily visualize Richard in a cell listening to the troubadour Blondel below. Near Vienna, we feasted in the home of a farmer who was celebrating with Gruner Veltliner (green wine, tastes like pinot gris) and the produce from their farms. And I think Vienna is as beautiful as Paris. In Italy, the drivers were crazy as always. They drove fast and seemed angry at anyone being ahead of them. But when the road shut down temporarily, everyone piled out of their vehicles to share wine and food. Then when the road reopened, the race began again. At the end of the summer term, David had already left for the States, and Londi and I drove to Zermatt, the village below the Matterhorn in the Swiss Alps. That was a fateful trip for both of us.
The trip was hair-raising for me in the Alps. I don't mind heights if I am on the ground but I was down on the floor boards in that car. Londi was driving and we were constantly above the timber line, with steep dropoffs onto 60 degree slopes, and never a guardrail, just flocks of sheep grazing precariously below. At the top of one mountain pass, we stopped, slapped hands together, and did a mock dance, so I could celebrate being alive. At Zermatt we rode the tram up the Matterhorn base and then got out to collect rocks. The Matterhorn is folded sediment which slid north in the collision and suturing of Italy (Adriatic Plate) with Europe (Euro-Asian plate) some 25 to 50 million years ago. It sits on top of oceanic crust in which the deep-sea basalts have been metamorphosed into pretty green serpentine. We were both loaded down with serpentine and Londi was standing near the edge of a clift. I asked her to marry me and she nearly fell off the edge, very dramatic. I knew how to spring a surprise on a lady.