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Debris-flow and flooding hazards associated with the December 1999 storm in coastal Venezuela and strategies for mitigation

Open File Report 01-0144

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Table 3. Comparison of depositional volume of debris flows worldwide. Magnitude M, equal to the logarithm of depositional volume in cubic meters, as proposed by Keaton et al. (1988) used for comparison.

 

Location

(Year)

M

Trigger

Reference

Rudd Canyon, Utah (1983)

 

Whitehouse Creek, California (1982)1

 

Fountain Green, Utah (1983)

 

Ophir Creek, Nevada (1983)2

 

Wollinitzbach, Austria (1966)

 

Campania, Italy (1998)3

 

Casita, El Salvador (1998)

 

Caraballeda, Venezuela (1999)

 

Malaya Almatinka River, Kazakstan (1921)

 

Nevados del Ruiz, Colombia (1985)

 

Mt. Ontake, Japan (1984)

 

Nevados Huascaron, Peru (1970)

 

 

Mt. Pinatubo, Philippines (1991)

 

Mt. St. Helens, Washington (1980)

4.8

 

5.1

 

 

5.2

 

5.2

 

5.5

 

6.2

 

6.3

 

6.3

 

6.5

 

 

7.2

 

 

7.5

 

7.7-8.0

 

8.9

 

9.4

Snowmelt

 

Rain

 

 

Snowmelt

 

Snowmelt

 

Rain

 

Rain

 

Rain

 

Rain

 

Rain

 

 

Volcanic explosion

 

Earthquake

 

Earthquake

 

 

Volcanic eruption

and rain4

Volcanic eruption

 

Keaton et al. (1983)

 

Wieczorek et al. (1987)

 

 

Lips and Wieczorek (1990)

Glancy and Bell (2000)

 

United Nations (1996)

 

Calcaterra et al. (2000)

 

Scott (2000)

 

This report

 

United Nations (1996)

 

 

United Nations (1996)

 

 

United Nations (1996)

 

Plafker and Ericksen (1978)

 

Newhall and Punongbayan (1996)

United Nations (1996)

 

1Evaluation of magnitude is based on volume of source landslide. Depositional volume is a minimum because of potential additional erosional contribution from channel.

 

2The trigger of this event was extremely complex involving landslide-induced flooding of a small lake and subsequent stream channel erosion (Glancy and Bell, 2000). The cited volume is only that part deposited on the fan.

 

3The volume represents the total deposition from debris flows onto about a half dozen fans.

 

4Volume represents total of lahar deposition within drainages of Mt. Pinatubo within first two months following major eruption. Typhoon Yunya during the eruption and subsequent typhoons and monsoons continued to generate flows with voluminous sediment deposits on fans for the next several years, so this figure represents only the initial debris flow volume from Typhoon Yunya.