Lent Reading List - Option 2: Earth's Critical Zones

Please note that if references are marked with an asterisk (*) , they have been highlighted by your lecturers as being particularly useful to you.

Journal References

If available online the journal title will be linked to ABSTRACT LEVEL. You will have the option to download full-text or pdfs.

A number of these references will be available in the part II/III reprint collection housed in the Library Office. A full listing of what is in this collection is available on the Library website.

Niels Hovius G2 2012

 

Lecture one


Beaumont, C, Fullsack, P., and Hamilton, J. (1992): Erosional control of active compressional orogens. In: McClay, K.R. (ed.), Thrust Tectonics, Chapman and Hall, London, 19-31.
Beaumont, C., Jamieson, R.A., Nguyen, M.H., and Lee, B. (2002): Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation. Nature, 414, 738-741.
Davis, D., Suppe, J., and Dahlen, F.A. (1983): Mechanics of fold-and-thrust belts and accretionary wedges. Journal of Geophysical Research, 88, 1153-1172.
Willett, S.D., Beaumont, C., and Fullsack, P. (1993): Mechanical model for the tectonics of doubly vergent compressional orogens. Geology, 21, 371-374.
Willett, S.D., Slingerland, R.L., and Hovius, N. (2001): Uplift, shortening, and steady state topography in active mountain belts, American Journal of Science, 301, 455-485.

Lecture 2

Hartshorn, K., Hovius, N., Dade, W.B., and Slingerland, R.L., 2002: Climate-driven bedrock incision in an active mountain belt. Science, 297, 2036-2038.
Howard, A.D., and Kerby, G., 1983: Channel changes in badlands. GSA Bulletin, 94, 739- 752.
Lave, f., and Avouac, J.P., 2001: Fluvial incision and tectonic uplift across the Himalayas of central Nepal. JGR Solid Earth, 106, 26561-26591.
Sklar, L.S., and Dietrich, W.E., 2001: Sediment and rock strength controls on river incision into bedrock. Geology, 29, 1087-1090.
Whipple, K.X., Hancock, G.S., and Anderson, R.S., 2000: River incision into bedrock: mechanics and relative efficacy of plucking, abrasion, and cavitation. GSA Bulletin, 112, 490-503.
Whipple, K.X., and Tucker, G.E., 1999: Dynamics of the stream-power river incision model: implications for height limits of mountain ranges, landscape response time scales, and research needs. JGR Solid Earth, 104, 17661-17674.

Lecture 3


Burbank, D.W., Leland J., Fielding, E., Anderson, R. S., Brozovic, N., Reid, M.R., and Duncan, C. (1996): Bedrock incision, rock uplift and threshold hillslopes in the northwestern Himalayas. Nature, 379, 505-510.
Densmore, A.L., Anderson, R.S., McAdoo, B.G., and Ellis, M.A. (1997): Hillslope evolution by bedrock landslides. Science, 275, 369-372.
Hovius, N., Stark, C.P., and Allen, P.A. (1997): Sediment flux from a mountain belt derived by landslide mapping. Geology, 25, 231-234.
Schmidt, K.M., and Montgomery, D.R. (1995): Limits to relief. Science, 270, 617-620.
Wolman, M.G., and Miller, J.P. (1960): Magnitude and frequency of forces in geomorphic processes. Journal of Geology, 68, 54-74.

Lecture 4

Brozovic, N., Burbank, D.W., and Meigs, A.J., 1997: Climatic limits on landscape development in the northwestern Himalaya. Science, 276, 571-574.
Fielding, E., Isacks, B., Barazangi, M., and Duncan, C., 1994: How flat is Tibet? Geology, 22, 163- 167.
Finlayson, D.P., Montgomery, D.R., and Hallet, B., 2002: Spatial coincidence of rapid inferred erosion with young metamorphic massifs in the Himalayas. Geology, 30, 219-222.
Montgomery, D.R., Balco, G., and Willett, S.D., 2001: Climate, tectonics, and the morphology of the Andes. Geology, 29, 579-582.
Zeitler, P.K., Meltzer, A.M., Koons, P.O., Craw, D., Hallet, B., Chamberlain, C.P., Kidd, W.S.F., Park, 5, Seeber, L., Bishop, M., and Schroder, J., 2001: Erosion, Himalayan geodynamics and the geomorphology of metamorphism. GSA Today, 11, 1.4-9.
 

Below, the refs are from previous years

Lecture 1 - 6    Dr Albert Galy

Recommended books

  • Allen, P.A. & Allen, J.R. Basin Analysis: principles and application: either 1990 or 2005 edition will do
  • FitzPatrick, E.A. Soils, Longman, London (1983).
  • Garrels, R.M. & Mackenzie, F.T. Evolution of sedimentary rocks New York (1971)
  • Ruddiman, W. & Prell, W. eds Global Tectonics and Climate Change, Plenum, New York (1997)

Lecture One

Dr A Galy 

Practical

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Lecture Two

Dr A Galy

Specific papers:

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Lecture Three

Dr A Galy

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Lecture Four 

Dr A Galy

Specific papers:
 

 

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Lecture Five

Dr A Galy

Lecture Six

Dr A Galy

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Lecture Seven

Niels Hovius

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Lecture Seven Practical

Niels Hovius

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Lecture Eight

Niels Hovius

 

Lecture Nine

  • Brozovic, N., Burbank, OW., and Meigs, A.J., 1997: Climatic limits on landscape development in the northwestern Himalaya. Science, 276, 57 1-574.
  • Fielding, E., Isacks, B,, Barazangi, M., and Duncan, C., 1994: How flat is Tibet? Geology, 22, 163-
  • 167.
  • Finlayson, OP., Montgomery, DR., and Hallet, 8., 2002: Spatial coincidence of rapid inferred erosion with young metamorphic rnassifs in the Himalayas. Geology, 30, 219-222.
  • Montgomery, DR., Balco, G., and Willett, S.D., 2001: Climate, tectonics, and the morphology of the Andes. Geology, 29, 579-582.
  • Zeitler, PlC, Meltzer, AM., Koons, P.O., Craw, 0., Hallet, B., Chamberlain, C.P,, Kidd, W.S.F., Park, 5, Seeber, L., Bishop, M., and Schroder, 3., 2001: Erosion, Himalayan geodynamics and the geomorphoiogy of metamorphism. GSA Today, 11, 1,4-9 

 

Lecture Ten

  • Beaumont, C, Fuilsack, P., and Hamilton, 1. (1992): Erosional control of active compressional orogens. j McClay, K.R. (ed.), Thrust Tectonics, Chapman and Hall, London, 19-31. 
  • Beaumont, C., Jamieson, R.A., Nguyen, M.H., and Lee, B. (2002): Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation. Nature, 414, 738-741. 
  • Davis, D., Suppe, 3., and Dahien, F.A. (1983): Mechanics of fold-and-thrust belts and accretionary wedges. Journal of Geophysical Research, 88, 1153-1172. 
  • Willett, S.D., Beaumont, C., and Fuilsack, P. (1993): Mechanical model for the tectonics of doubly vergent cornpressional orogens. Geology, 21, 371-374. 
  • Willett, S.D., Slingerland, R.L., and Hovius, N. (2001): Uplift, shortening, and steady state topography in active mountain belts. American Journal of Science, 301, 455-485.

 

Lecture Eleven

  • Carter L. et al, 2002: Source, sea level and circulation effects on the sediment flux to the deep ocean over the past 15 ka off eastern New Zealand. Global and Planetary Change, 33, 339-355.
  • Crosby B.T and Whipple K.x., 2006: xniclcpoint initiation and distribution within fluvial networks: 236 waterfalls in the Waipaoa River, North Island, New Zealand. Geomorphology, 82, 16-38.
  • Eden D.N. and Page MI,, 1998: Palaeoclimatic implications of a storm erosion record from late Holocene lake sediments, North Island, New Zealand. Palaeogeography, Palaeoclimatology, Palaeoecology, 139, 37-58.
  • Gomez B. et at., 1998: Floodplain construction by recent, rapid vertical accretion: Waipaoa River, New Zealand. Earth Surface Processes andLandforms, 23, 405-413.
  • Gomez B. et at., 2002: Self-organized criticality in layered, lacustrine sediments formed by landsliding. Geology, 30,
  • 5 19-522.
  • Gomez B. et at., 2004: El Nino-Southem Oscillation signal associated with middle Holocene climate change in Interconnected terrestrial and marine sediment cores, North Island, New Zealand. Geology, 32, 653-656.
  • Gomez B. et al., 2007: A 2400 yr record of natural events and athropogenic impacts in intercorrelated terrestrial and
  • marine sediment cores: Waipaoa sedimentary system, New Zealand. Geological Society of America Bulletin, 119, 1415-
  • 1432.
  • Hicks D.M. et aI., 2000: Erosion thresholds and suspended sediment yields, Waipaoa River basin, New Zealand. Water Resources Research, 36, 1129-1142.
  • Hicks D.M. et al., 2004: Event suspended sediment characteristics and the generation of hyperpycnal plumes at river mouths: East Coast Continental Margin, New Zealand. Journal of Geology, 112, 461-485.
  • Kettner Al. et al., 2007: Modeling suspended sediment discharge from the Waipaoa River system, New Zealand: The last 3000 years. Water Resources Research, 43, W07411, doi:10,1029/2006WR005570.
  • Marutani T. et al., 1999: Influence of storm-related sediment storage on the sediment delivery from tributary catchments in the upper Waipaoa River, New Zealand. Earth Surface Processes and Landforms, 24, 88 1-896.
  • Page MI. et al., 1994: Sediment budget to assess the geomorphic effect of a cyclonic storm, New Zealand. Geomorphology, 9, 169-188.
  • 0rpm A.R., 2004: Ijolocene sediment deposition on the Poverty-slope margin by the muddy Waipaoa Tiver, East Coast New Zealand Journal of Geology, 209, 69-90.
  • Trustrum NA. et a]., 1999: Sediment production, storage and output: the relative role of large magnitude events in steepland catchments. Zeitschrfflfur GeomorphologieN.F., 115,71-86.
  • Walsh 1.1’. et at., 2007: Demise of a submarine canyon? Evidence for highstand infilling on the Waipaoa River continental margin, New Zealand. Geophysical Research Letters, 34, L20606, doi:10.l029/2007GL031142.

 

Lecture Twelve

 

Lecture Thirteen

 

Lecture Fourteen

Sasha Turchyn

General reading for lectures 14 to 16

Lecture Fifteen


 

Lecture Sixteen

Sasha Turchyn

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Last updated on 20-Sep-12 13:30