| GEOG/GEOL
4241:
Principles of
Geomorphology Lecture: TTh 11-12:15 PM Lab: T 2-4:50 PM Instructor: John Pitlick TA: Erich Mueller |
Course Goals: This course
emphasizes earth-surface
processes and methods used to interpret the origin of landscapes.
Surface processes are constantly at work, shaping and re-shaping the
Earth's topography. Living in Boulder we are particularly lucky,
because the surrounding areas offer excellent opportunities to study
geomorphology; examples of landforms formed by glaciation, weathering,
landslides, streamflow, and wind all occur within a few hours drive of
here. To take advantage of these opportunities, we plan on taking
a number of field trips where we will test theoretical models of
erosion and sediment transport. The field trips and lab exercises
will provide you with "hands-on" experience, and broad-based exposure
to the various field and analytical techniques used in studying
geomorphic processes.
Text: Process Geomorphology by D.F. Ritter, R.C. Kochel, and J.R. Miller
Lab: A 3-hour lab session will be held every Tuesday. Roughly half of the labs will involve field trips in which you will learn some of the basic techniques used in geomorphology. An all-day field trip to Arapaho Pass to view alpine and glacial landforms is scheduled for Saturday, Sept. 8; a half-day field trip to eastern Colorado may be scheduled later in the semester. A small notebook will be useful for field trips. When we don’t go in the field, we will complete map-based or computer-oriented exercises. You should bring pencils, calculator, engineers scale, and a protractor to each lab.Exams will cover material from the lectures text, and readings. Test questions will be short answer and essay. Under certain circumstances, you may take an exam early (e.g. because of a religious holiday). However, you cannot take an exam late- if you miss an exam, you must first provide a legitimate excuse, such as a written note from a doctor; I will then give you a score equal to your grade on the other midterm. No make-up exams will be given, regardless of your personal situation (illness, death in the family, whatever). If you cannot explain your reason for missing an exam, you will receive a score of zero for that exam.
- 1st midterm 20 % (tentatively scheduled for Sept. 27)
- 2nd midterm 20 % (tentatively scheduled for Nov. 1)
- Final exam 20 % (equal to a midterm; exam scheduled for Saturday, Dec. 15)
- Lab exercises 40 %
Dates |
Topics |
Reading |
| 28 Aug | Introduction & Basic Principles |
Chapter 1, 9 |
| 30 Aug | Glaciers I: Formation of Ice, Mechanics of Flow, Mass Balance |
Chapter 9,10 |
| 4-6 Sep | Glaciers II: Erosion, Transportation, and Deposition | Chapter 10, Field Trip, Sept. 8 |
| 11-13 Sep |
Quaternary Record of Climate Change | |
| 18-25 Sep | Chemical Weathering and Soils | Chapter 3 |
| 27 Sep | Midterm Exam I | |
| 2-11 Oct | Hillslope Processes | Chapter 4 |
| 16-18 Oct | Drainage Basins | Chapter 5 |
| 23-30 Oct |
Flow and Sediment Transport in Rivers |
Chapter 6 |
| 1 Nov |
Midterm Exam II | |
| 6-8 Nov |
Channel Morphology |
|
| 13-15 Nov | Fluvial Adjustments to Environmental Change | Chapter 7 |
| 19-23 Nov |
Thanksgiving Break |
|
| 27-29 Nov |
Regional Uplift and Denudation | Reserve Reading |
| 4-6 Dec | Integration of concepts and review |
|
| 11 Dec | Last Day of Classes (for us) |
|
| 15 Dec | Final Exam, 10:30 AM -1:00 PM |
Lab Exercises and Field Trips (more or less in this order):
1. Review of topographic maps, cross sections, calculations, etc.2. Glacial mass balance; erosion and deposition
3. Glacial and periglacial processes, field trip, Saturday, Sept. 8
4. Hillslope measurements
5. Computer exercise: analysis of hillslope profiles6. Debris flows
7. Drainage network analysis
8. Channel morphology and sediment movement
9. Hydraulic geometry
10.
Magnitude/Frequency analysis
11. Eolian deposits (sand dunes) of eastern Colorado
12. Cenozoic erosion
surface/geomorphic history
of
the Front Range
Below are some questions illustrating the format of one of my
exams.
You have 1 hour for this test. Spend time on questions that are worth the most. Think about the question before writing anything and then give a short, concise answer; drawn-out discussions will not earn you points. If you write out a formula, be sure to define any terms. Good luck.
1. Give a concise, one sentence, definition for each of the following terms (4 pts. each):
a) sublimation
c) leaching
d) a 2 to 1 clay
e) cation exchange
2. Explain why a change in equilibrium line altitude (ELA) due to a
change in climate may have a greater effect on ice sheets than valley
glaciers.
Assume the change in ELA is the same for both (10 pts.):
3. Glen's law is written as strain rate = coefficient x shear stress ^ n
where is the ________________________________ , t is the _______________________________ , a is a coefficient, and n is an exponent with a mean value of about ______ . For this value of n, a doubling of t would cause a(n) ______ -fold increase in (8 pts.).
a) explain with reference to eqn. 1 why the value of t at the
base of most glaciers is ~100 kPa (4 pts.):
b) explain with reference to eqn. 1 why crevasses seldom
propagate
to depths of more than 30m (4 pts.):
4. Polar glaciers differ from temperate glaciers in a number of
respects.
As briefly as you can, contrast the differences between (a) processes
of
ice formation, including the role of water; (b) physical properties of
the ice; (c) mechanisms of movement; and (d) debris entrainment in
polar
vs. temperate glaciers (16 pts.):