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Welcome to Desert Geology, one of our "Special Topics" under Geology 350. This course is designed to introduce the geological processes which form and operate in the deserts of the world. The centerpiece of our section this semester is a Spring Break field trip to the Mojave Desert. The first half of the course will be preparation for the trip, and the second half will be analysis, discussion and review of what we saw and found. This is a half-credit course so we will formally meet for roughly half the time of a regular course (except for the six-day field trip!) and generally do half the work. All the assignments involve writing, presenting and discussing -- no tests or quizzes. Please see the course notes at the end of this syllabus. You will also see that this course is taught with the help of my colleagues Greg Wiles, Brennan Jordan, and Jeanne Fromm. They will present material in class and help lead the spring field trip. This syllabus is also a newsletter and web resource for the course. It will be updated at least once a week with relevant links and geological news items. Please check it often. Several of our reading assignments will be web-only. Teaching a course on the geology of deserts has been a dream of mine for years. I hope you enjoy it as much as I do!
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Introduction to Deserts of the World |
| Reading: USGS Online Desert Booklet (please read all pages) | |
| Special Events: | |
| Assignments: | |
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Web Resources for Week #1: Deserts are extraordinary. I must tell you from the beginning that deserts are my natural environment. The world for me consists of dry, brown, dusty hills where I can see for miles under a brilliant sky. A place so dry the air plucks at your lips and the sand crackles under your feet. And there is always the wind and the sun. Every landscape is quickly divided into the shady and the sunlit, the wind-swept and the protected. The rest of the world with its trees and grass, rivers and lakes, clouds and rain, is an exception for me. The Mojave Desert is my homeland. I grew up in Barstow, California. Rainbow Basin, shown in this wonderful 360-degree photo, is where I had many childhood adventures. I have a passion for deserts, so teaching this course is a rare privilege for me. During this first week we will discuss the general setting of deserts and the basic geological processes which operate within them. Our initial definition of a desert is the simplest one: a place which receives less than 25 cm (10 inches) of precipitation a year. Deserts can be hot or cold (they are rarely moderate!), they can be filled with life or virtually lifeless (or actually lifeless if we consider Martian deserts), and they can be flat or mountainous. We will be considering the "non-polar" deserts, especially the large ones like the Sonoran, Sahara, Arabian, Atacama, Kalahari, Australian, Gobi, and many more which are lesser known (including the Negev in Israel where Wooster geologists have recently been working). We will often return to the starkly beautiful Death Valley of southern California. Geology in the News:
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Introduction to the Mojave Desert (Geology and History) |
| Reading: S&G pages 1-17; East Mojave Geology (print pdf) | |
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| Web Resources for Week #2: Our topic for this day is almost impossible to summarize in a couple of web-paragraphs. I will briefly outline the geological history of the Mojave Desert, leaving plenty of room for Dr. Jordan to talk about the tectonic and structural context of the Mojave next week. The link to the summary of East Mojave Geology in the reading assignment is simply a time chart showing the major geological events in a complex region. We won't talk about them all! I will spend most of the period talking about the human history of the Mojave Desert. It in many ways is even more complex than the geology, and it is full of drama, bravery, cruelty, cowardice, creativity, surprises and mysteries -- like most history! The primary characters will include the Mojave Indians, Francisco Garces, the first of the "Spanish Fathers" (as they were always called in my California History classes of childhood), Jedediah Smith (one of my heroes), The Old Spanish Trail, emigrant wagon trains, outlaws, the railroads, the mining industry, Route 66, and much else. Patrice and I have also worked out a system for collecting the $500 field trip fee. Please make out a check to "The College of Wooster" for this amount, write "Mojave Field Trip" on your memo line, and then give it to Patrice before February 25. Geology in the News:
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Tectonic and Structural Context of the Mojave Desert |
| Reading: S&G pages 67-78; 87-98; handout from Dr. Jordan | |
| Special Events: | |
| Assignments: Research project topics due in class | |
| Web Resources for Week #3: Dr. Brennan Jordan is our lecturer this week. He will be discussing the general geological framework of western North America, in particular the Cordilleran Orogen. The Basin and Range province is characterized by extraordinary extensional processes that we still do not fully understand. Many of these observations and ideas will be directly applicable to what we see in the Mojave Desert, and some will be important to know as part of our larger picture of western US geology. Geology in the News:
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The Ever-Present Wind: Dunes, Ventifacts and Other Geological Results |
| Reading: S&G pages 99-105; 128-138 | |
| Special Events: | |
| Assignments: At least two new references for your research project, along with a project title, are due on Monday in class. See the recent e-mail from me. | |
| Web Resources for Week #4: The wind is the part of the desert that I miss the most. There is something primal in the desert wind, the way it can go from a light, caressing breeze to hot breath to a raging dust storm in just minutes. The features the wind creates are among the most attractive images in geology. ( "Of all natural forms, sand dunes are the most elegant - so simple, severe, bare. Nature in the nude." From Desert Images, by Edward Abbey.) Our goal for Monday's lecture is to understand the wind in the desert: where it comes from and what it does as a geological process. We'll start with an overview of eolian (wind) processes, which this physical geography webpage gives us (more or less). What causes the wind in the first place? How do Mojave Desert winds differ from other wind systems? (OK, that poem isn't so great, but at least you were entertained by the pop-ups. Maybe this Mojave poem by Sylvia Plath is better?) How windy is it in the Mojave Desert right now? As for the effects of wind in the desert, you'll certainly want to start with some movies of sand movement in wind tunnels (very exciting, especially the close-ups), and read how some Germans have modeled sand dunes in that classic German way of theirs. As for real sand dunes, there are many websites with spectacular photos and descriptions, several emphasizing the geology of sand dunes. We will even see one of the famous deposits of "acoustic sands" on our field trip. (Hearing them is another story. I've never heard the "booming" they sometimes produce.) The movement of sand in deserts is a serious issue, especially when desertification approaches a city, like Nouakchott, Mauritania, in this example. Finally, we'll look at the issue of dust derived from deserts by the wind. Loess is a deposit of wind-blown silt or clay. (Click on that link and then the little sound icon to hear someone authoritatively misprounounce it.) Dust storms have increased in frequency across the globe as deserts have increased and desert soils have been disturbed. This has very worrying health implications. Desert dust storms are even implicated in the decline of coral reefs. We will, thankfully, feel only the very healthy Mojave wind on our field trip this spring. Geology in the News:
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Moving Water: Alluvial Fans, Debris Cones and Wadis of the Mojave |
| Reading: S&G pages 54-65; 106-118; 139-151 | |
| Special Events: | |
| Assignments: Essay #1 due in class on Monday | |
| Web Resources for Week #5: Deserts are usually such dry places that when rain does come it can bring dramatic effects. Desert soil can shed water quickly, and there are relatively few plants to retard runoff. The result is often a flash flood. Here is a NOAA fact page on predicting flash floods, not all of which are in deserts (thanks in part to deforestation), and here is a NOAA page where you can get the latest flash flood warnings. And please, young geologists, never end up in a narrow canyon during a flash flood. Alluvial fans and debris cones (3-D photo!) are dramatic water-formed features, and they are well displayed in deserts. They are characterized by their fan shapes (they are really deltas on land) and their poorly-sorted sediments. On our field trip we will see that wadis (also known as arroyos, washes, or dry river beds) will be our pathways into the desert wilderness. Here's a USGS page about wadi (wash) development in the Mojave. Note how important it is to understand past climate conditions and geomorphology before interpreting present geomorphic features. This is especially true for the Mojave River, which you will soon get to know well. Want to see more 3-D photographs of Death Valley? They are very cool. We have plenty of the required glasses in Scovel if you want to borrow a pair. Remember that your Essay #1 is due in class on Monday. Geology in the News:
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Standing Water: The Geology of Playas |
| Reading: S&G pages 33-53; 160-173 | |
| Special Events: Field trip deposit due on Friday to Patrice | |
| Assignments: Rewritten Essay #1 due in class | |
| Web Resources for Week #6: This week we will finish our discussion of moving water in deserts, and then look at the features which result when that water comes to rest on valley floors. Playas are dry lake beds in closed desert basins. Water reaches them infrequently, and when it does it brings clay and silt and many exotic dissolved minerals. Playa means "beach" in Spanish, which doesn't make much sense to me. In Latin America the Spanish-speakers call them salars ("salt flats"). There are many geological processes on and around playas we will discuss, and I can't resist mentioning that playas are fine places for racing rocket cars, landing aircraft, testing alien spacecraft, firing rockets, and the Burning Man festival. To demonstrate the utility of modern playas, even the U.S. Army has a page on them. On our field trip to the warm and dry Mojave Desert, we will be staying on the shore of Soda Lake, a playa at the end of the Mojave River. There is a reason why it is called "soda" lake, of course, and that is because of the wide variety of exotic evaporative minerals in the playa deposits. One of the richest sites for the mineral borax is near Trona, California, on the large and ancient playa now called Searles Lake with its fantastic associated "pinnacles". Here is a superb 360-degree view of the Trona Pinnacles. Ironically, in southern California there was more value in these colorless evaporative minerals than in gold. Of course, we will also visit Racetrack Playa and try our hand at guessing why rocks mysteriously move across its surface. If you want detailed information about those exotic playa minerals borax, ulexite and trona, you know where to click! (These sites have excellent interactive crystallographic diagrams. I don't know what to do with them, but they're fun!) Don't forget about the $500 check for the field trip. It is due by Friday, February 25, to Patrice. Geology in the News:
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Pleistocene History of the Mojave Desert |
| Reading: S&G pages 41-53 | |
| Special Events: Airline tickets distributed in class | |
| Assignments: | |
| Web Resources for Week #7: The Pleistocene Mojave Desert was not, much of the time, a desert at all. This week we will look in detail at the pluvial lakes which were common in the Mojave and throughout the intermountain west. The vast playas we see today are remnants of these lakes, as are the massive alluvial fans and pediment surfaces. An important lesson gained from studying the Pleistocene history of the Mojave area is that the present landscape is not in equilibrium with present geological processes. Much of what we see is a vestige of the later Pleistocene. This should not be surprising considering that the desert we know today has only been in existence for about 14,000 years. We will concentrate in this week's lecture on the history of the lakes associated with the Mojave River. The incision of Afton Canyon is a controversy. Was it cut catastrophically in a flood from Lake Manix to Lake Mojave? Or was it cut more gradually? The difference is that one school supports a flood which could have occurred in little more than ten hours, while the other is looking at thousands of years. I favor the quick model because the arguments for it seem better. We can test it out ourselves in the field because we will be living right next to this beautiful canyon. (Oh I love this photo!) There are also biological vestiges from the cooler and wetter Pleistocene times in the Mojave. The most charismatic organisms we'll look at in this regard are the desert pupfish which are now geographically and genetically isolated in small populations after their lake environments disappeared. We will also examine the distributions of creosote bushes and Joshua trees to see how they too indicate climate change since the Pleistocene. Will we see a fantastic wildflower show on our Mojave trip? March is the best time. The question is whether the Mojave has had too much rain this winter. You can check out the current weather in Barstow as we prepare for yet another snowstorm this week in Wooster. Sigh. Check out this photograph taken last week at Badwater on the floor of Death Valley. Can you believe it? Boating in Death Valley? I've never seen anything like it. Record rainfall this month. Thanks to Dr. Jordan for sending me the link. Geology in the News:
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Introduction to the Field Trip Locations and Projects |
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| Special Events: Mojave Desert Field Trip is March 19-25 | |
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| Web Resources for Week #8: It has been much fun for us working out the plan for our Mojnave Desert field trip less than two weeks from now. In class we will discuss the following stops and other activities. Of course, this is all an estimate subject to change because of weather, flooding (I never thought I'd have to say this!), resources, and our developing interests. Our objective is simply to explore as much of the Mojave as we can. Be sure to bring to class your completed Information Sheet and the Sharp & Glazner guidebook. Here are the days and their projected events -- Saturday, March 19: Arrive in Las Vegas at 10:45 a.m. We'll be out of that strange city by noon, probably eating a fast food lunch on its outskirts. Our first geological stop will be at Red Rocks Canyon National Conservation Area just outside the city. Here we'll see beautiful Mesozoic sandstones and a tremendous thrust fault. (I did my dissertation in the Spring Mountains above.) We'll then drive to our lodgings at the Desert Studies Center on the shore of Soda Dry Lake. We'll spend the rest of the day exploring our new neighborhood. Sunday, March 20: Our objective on this day is to explore the southern portion of Death Valley National Park. We plan to hit as many interesting sites as we can as far north as the Furnace Creek Visitor Center. This will include the turtlebacks, Shoreline Butte (if we can get there across the renewed Lake Manly), lots of beautiful alluvial fans, faults, and ventifacts. Monday, March 21: Time to see Manix Lake and the beautiful stratigraphy and structures around (yes) Barstow. We will start early in the morning (of course! don't think you're sleeping in!) and work our way through the ancient lake beds moving west. I hope we can have lunch in the extraordinary Rainbow Basin north of downtown Barstow. On the way we plan to see examples of folds, faults and detachment structures. On the way back we will visit Afton Canyon and look for evidence of the draining of Manix Lake. Tuesday, March 22: This will be a long driving day, but well worth it. Again we will head west, passing near Barstow and through Ridgecrest. Our goal is to visit the Trona Pinnacles. Wednesday, March 23: Not as much driving this day as we head south and east into the Mojave National Preserve. So much to see here. On the way to the Kelso Dunes we will stop and look at some Cambrian limestones with trace fossils and oncolites. We will visit the broad and large Cima Dome, the Granite Mountains (check out the associated geologic map), and the incredible volcanism at Hole in the Wall. (I can hardly sit still to write all this. What a cool trip this will be.) Thursday, March 24: This is our catch-up day. We'll look at the Tecopa lake beds and volcanic ashes, the tuff at Resting Springs Pass, and the Amargosa Chaos outside Death Valley at Exclamation Rock. Friday, March 25: We'll be up early to drive back to Las Vegas, drop off our rental vehicles and board the 11:10 a.m. flight back to Cleveland. The weather will be perfect for our last view of the Mojave Desert. Geology in the News:
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Summary of the Field Trip Observations and Other Adventures |
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| Assignments: Please bring collected specimens to class. | |
| Web Resources for Week #9: Here are the first photographs I have to post of our wonderful field trip last week. We'll have more and better photographs later. For today's class, please bring in the specimens you collected on the trip. We'll review our journey and the many things we saw, then talk about how we can further study some of our samples. The staff of the Desert Studies Center, by the way, had the highest compliments for our group. They enjoyed your enthusiasm, humor, and the care you showed the staff and the facilities. I am very proud of Wooster geology students -- with good reason. Geology in the News:
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Student Research Presentations: Elyse and Monica |
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| Assignments: Essay #2 is due in class | |
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Geology in the News:
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Student Research Presentations: Kaylin and Anton |
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| Special Events: Osgood Lecture: Dr. Tricia Kelley of the University of North Carolina, Wilmington, presents "Evolution and Creation: Conflicting or Compatible?" (Lean Lecture Room, 8 p.m., April 14) | |
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| Web Resources for Week #11: Kaylin (extension in the Mojave) and Anton (flash floods) are our speakers this week. Geology in the News:
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Student Research Presentations: Kamilla |
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| Web Resources for Week #12: Kamilla is our speaker this week. Her topic is hydraulic mining. Geology in the News:
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Student Research Presentations: Erica, Ryan and Kate |
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| Web Resources for Week #13: The last of our student presentations: Erica (recent volcanism in the Mojave), Ryan (the effects of livestock on erosion) and Kate (archaeology of the Mojave Desert). Geology in the News:
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Sorting out the last issues |
| Reading: | |
| Special Events: We meet at 2:00 p.m. instead of the usual 1:00 p.m. | |
| Assignments: Research paper is due in class at 2:00 p.m. | |
| Web Resources for Week #14: Our last day! All we are doing is collecting the research papers and distributing the course evaluation forms. We'll also remember that wonderful field trip ... Geology in the News:
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Since this is a half-credit course we will expect to do about half the work of an ordinary advanced geology course. That is if we don't count all that time on the field trip! (Which will be so much fun.) Here are the primary elements of this course: Field trip.--The Mojave Desert field trip is the most important thing we will do. It is where we'll actually see what we've been talking about, and you will also be collecting resources on this trip for your own research projects. Our plans are to leave Cleveland-Hopkins airport on Saturday, March 19, and return to Cleveland-Hopkins on Friday, March 25. We can transport you from Wooster to the airport and back, but if you're coming from somewhere else you'll need to make those arrangements on your own. The trip begins with a flight to Las Vegas (which will give some of you your first views of the desert southwest). Once there we will rent vans and drive into southeastern California, staying at the Desert Studies Center, a field station near my hometown of Barstow. From that base we will explore Death Valley and other parts of the eastern Mojave Desert. Each student will have a particular research topic related to some aspect of desert geology we will see on the trip. Most of the expenses for this trip will be paid out of endowed funds in the Geology Department. All that we require from you is $500 to partially cover transportation costs. This fee must be paid before the trip. Writing and speaking.--This is a writing course and so we will fill the requirements with a series of diverse writing assignments, discussion of scientific writing, and peer review. You will have at least two short essays on topics related to desert geology which appear in the news or recent scientific literature. These will be assigned in the middle and end of the semester. You will also have a research paper roughly 10-15 pages long on a topic of desert geology related to our field trip. (Be sure to see our departmental writing guide.) This research paper will also be the basis of a class presentation you will give in the last part of the semester. We will discuss these assignments in more detail in class. Note that there are no tests, no quizzes, and no final examination. Participation.--Desert Geology meets once a week (Mondays, 1-2:20 p.m., Scovel 216). I will expect you to be present at each lecture, to do the assigned readings, and to ask and answer questions. I will also expect you to be active participants on the field trip. This participation will be 10% of your final grade. I don't think we'll have any problems with this -- you all have an "A" in participation unless you show me otherwise.
Sharp, R.P. and Glazner, A.F. 1997. Geology Underfoot in Death Valley and Owens Valley. Mountain Press Publishing Company (Missoula, Montana), 321 p. [Readings are listed in the lecture outline as "S&G".] Note that we also have some required readings from the Web. These are linked in the "reading" category of the relevant weeks in the syllabus.
Course Instructor I have a weekly appointment schedule posted outside my office door in Scovel. Please sign up for an appointment if you have any questions or just want to talk.
Photo of the Kelso Dunes by Brennan Jordan. Scovel 120 Telephone ext. 2247 mwilson@wooster.edu |