Skip to main content

Tree-Ring Dated Landslide Movements and Seismic Events in Southwestern Montana, USA

  • Chapter
  • First Online:
Tree Rings and Natural Hazards

Part of the book series: Advances in Global Change Research ((AGLO,volume 41))

Abstract

Because many tree species can live for several centuries or longer (Brown 1996), tree-ring analysis can be a valuable tool to date geomorphic events such as landslides, earthquakes, and avalanches in regions lacking long historical records. Typically, a catastrophic landslide will destroy all trees on the landslide, but trees on slower moving landslides may survive. For example, the Slumgullion earthflow, in southwestern Colorado, moves 0.5–5.5 m annually, yet is covered by aspen (Populus tremuloides) and conifers (Baum and Fleming 1996). Trees that survive such movements undoubtedly suffer damage, such as topping, tilting, impact, or root breakage. This damage is commonly recorded in the tree-ring record and analysis of this record can be used to reconstruct past landslide activity.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 169.00
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 219.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 219.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

References

  • Baum R, Fleming R (1996) Kinematic studies of the Slumgullion landslide, Hinsdale County, Colorado. In: Varnes D, Savage W (eds) The Slumgullion earth flow: a large-scale natural laboratory. US Geol Surv Bull 2130: 9–12

    Google Scholar 

  • Bekker M (2004) Spatial variation in the response of tree rings to normal faulting during the Hebgen Lake earthquake, southwestern Montana, USA. Dendrochronologia 22(1):53–59

    Article  Google Scholar 

  • Brown P (1996) Oldlist: a database of maximum tree ages. In: Dean J, Meko D, Swetnam T (eds) Tree rings, environment, and humanity. Radiocarbon pp. 727–731

    Google Scholar 

  • Carrara P (1979) The determination of snow avalanche frequency through tree-ring analysis and historical records at Ophir, Colorado. Geol Soc Am Bull 90(8):773–780

    Article  Google Scholar 

  • Carrara P (2002) Response of Douglas-firs along the fault scarp of the 1959 Hebgen Lake earthquake, southwestern Montana. Northwest Geol 32:54–65

    Google Scholar 

  • Doser D (1985) Source parameters and faulting processes of the 1959 Hebgen Lake, Montana, earthquake sequence. J Geophys Res 90(B6): 4537–4555

    Article  Google Scholar 

  • Fritts H (1976) Tree rings and climate. Academic Press, New York

    Google Scholar 

  • Fuller M (1912) The New Madrid earthquake. US Geol Surv Bull 494

    Google Scholar 

  • Jacoby G Jr, Sheppard P, Sieh K (1988) Irregular reoccurrence of large earthquakes along the San Andreas fault: evidence from trees. Science 241(4862):196–199

    Article  Google Scholar 

  • Jensen J (1983) The Upper Gros Ventre landslide of Wyoming-A dendrochronology of landslide events and possible mechanics of failure. Geol Soc Am Abstr 15(5):387

    Google Scholar 

  • Jibson R, Keefer D (1988) Landslides triggered by earthquakes in the central Mississippi Valley, Tennessee and Kentucky. US Geol Surv Prof Paper 1336-C: 1-24

    Google Scholar 

  • Keefer D (1984) Landslides caused by earthquakes. Geol Soc Am Bull 95(4):406–421

    Article  Google Scholar 

  • LaMarche V Jr, Hirschboeck K (1984) Frost rings in trees as records of major volcanic eruptions. Nature 307(5947):121–126

    Article  Google Scholar 

  • Logan R, Schuster R (1991) Lakes divided – The origin of Lake Crescent and Lake Sutherland. Clallam County Washington Washington Geology 19:38–42

    Google Scholar 

  • Luikart EJ (1997) Syn- and post-Laramide geology of the south-central Gravelly Range, southwestern Montana. Montana State University, M.Sc. Thesis

    Google Scholar 

  • McGee W (1893) A fossil earthquake. Geol Soc Am Bull 4:411–414

    Google Scholar 

  • Meisling K, Sieh K (1980) Disturbance of trees by the 1857 Fort Tejon earthquake, California. J Geophys Res 85(B6): 3225–3238

    Article  Google Scholar 

  • O’Neill J, LeRoy T, Carrara P (1994) Preliminary map showing Quaternary faults and landslides in the Cliff Lake Quadrangle, Madison County, Montana. US Geol Surv Open-File Rep 94-198, scale 1:24,000

    Google Scholar 

  • Panshin A, de Zeeuw C (1970) Textbook of wood technology, 3rd edn. McGraw-Hill, New York

    Google Scholar 

  • Pardee J (1926) The Montana earthquake of June 27, 1925. US Geol Surv Prof Paper 147-B

    Google Scholar 

  • Qamar A, Stickney M (1983) Montana earthquakes 1869–1979, historical seismicity and earthquake hazard. Montana Bureau of Mines and Geology, Memoir 51

    Google Scholar 

  • Reeder J (1979) The dating of landslides in Anchorage, Alaska – A case for earthquake-triggered movements. Geol Soc Am Abstr 11(7):501

    Google Scholar 

  • Scott H (1936) The Montana earthquake of 1935. Montana Bureau of Mines and Geology, Memoir 16

    Google Scholar 

  • Sheppard P, Jacoby G (1989) Application of tree-ring analysis to paleoseismology: two case studies. Geology 17(3):226–229

    Article  Google Scholar 

  • Shroder J Jr (1978) Dendrogeomorphological analysis of mass movement on Table Cliffs Plateau, Utah. Quat Res 9(2):168–185

    Article  Google Scholar 

  • Smith R, Sbar M (1974) Contemporary tectonics and seismicity of the Western United States with emphasis on the Intermountain seismic belt. Geol Soc Am Bull 85(8):1205–1218

    Article  Google Scholar 

  • Stickney M, Bartholomew M (1987) Seismicity and late Quaternary faulting of the northern Basin and Range Province, Montana and Idaho. Bull Seismol Soc Am 77(5):1602–1625

    Google Scholar 

  • Stokes M, Smiley T (1968) An introduction to tree-ring dating. University of Chicago Press, Chicago

    Google Scholar 

  • Stover C, Coffman J (1993) Seismicity of the United States, 1568-1989 (Revised). US Geol Surv Prof Pap 1527

    Google Scholar 

  • Walpole R, Myers R (1992) Probability and statistics for engineers and scientists, 4th edn. MacMillan, New York

    Google Scholar 

  • Williams P, Jacoby G, Buckley B (1992) Coincident ages of large landslides in Seattle’s Lake Washington. Geol Soc Am Abstr 24(5):90

    Google Scholar 

  • Witkind I, Stickney M (1987) The Hebgen Lake earthquake area. In: Beus S (ed) Centennial Field Guide, Rocky Mountain Section, Geol Soc Am, Boulder, pp 89–94

    Chapter  Google Scholar 

Download references

Acknowledgments

The authors thank L.W. Anderson, R.A. Crovelli, H.C. Fritts, T.C. Hanks, D.K. Keefer, and D.R. Lageson whose knowledge and ideas contributed to this paper. Previous versions of this manuscript benefited from reviews by F.C. Brunstein, D.R. Butler, J.R. Giardino, H.L. Goldstein, K.M. Haller, and J.S. Pigati, and an anonymous reviewer

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Paul E. Carrara .

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2010 Springer Science+Business Media B.V.

About this chapter

Cite this chapter

Carrara, P.E., O’Neill, J.M. (2010). Tree-Ring Dated Landslide Movements and Seismic Events in Southwestern Montana, USA. In: Stoffel, M., Bollschweiler, M., Butler, D., Luckman, B. (eds) Tree Rings and Natural Hazards. Advances in Global Change Research, vol 41. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-8736-2_39

Download citation

Publish with us

Policies and ethics