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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Jeffrey A. Coe</dc:contributor>
  <dc:contributor>Manuel Mota Chavarria</dc:contributor>
  <dc:contributor>Jonathan W. Godt</dc:contributor>
  <dc:contributor>Arthur C. Tarr</dc:contributor>
  <dc:contributor>Lee-Ann Bradley</dc:contributor>
  <dc:contributor>Sharon A. Rafferty</dc:contributor>
  <dc:contributor>Dean Hancock</dc:contributor>
  <dc:contributor>Richard L. Dart</dc:contributor>
  <dc:contributor>Margo L. Johnson</dc:contributor>
  <dc:creator>Robert C. Bucknam</dc:creator>
  <dc:date>2001</dc:date>
  <dc:description>The torrential rains that accompanied&#13;
Hurricane Mitch in October and November&#13;
of 1998 triggered thousands of landslides in&#13;
the moderate to steep terrain bordering the&#13;
Motagua and Polochic Rivers in eastern&#13;
Guatemala. Using aerial photographs taken&#13;
between January and March 2000 we&#13;
mapped all visible landslides larger than&#13;
about 15 m in minimum dimension in a&#13;
study area of 10,000 km2 encompassing&#13;
twenty 1:50,000-scale topographic map&#13;
quadrangles.&#13;
Rainfall from Hurricane Mitch was&#13;
exceptional because it was geographically&#13;
widespread, prolonged over a period of&#13;
about a week, moderate to heavy in intensity,&#13;
and occurred at the end of the rainy season&#13;
when the ground already had a high&#13;
moisture content. As documented in this&#13;
report, this type of rainfall, on saturated or&#13;
nearly saturated ground, has the capability to&#13;
trigger both shallow and deep-seated landslides&#13;
over a large area.&#13;
We mapped about 11,500 landslides in&#13;
the study area. The mapped landslides were&#13;
of two general types: relatively small, translational&#13;
and rotational landslides that commonly&#13;
mobilized into debris flows and covered&#13;
less than several hectares in area (not&#13;
including flow paths), and large, commonly&#13;
translational, landslides that sometimes generated&#13;
debris flows and covered between&#13;
15 ha and 25 ha (not including flow paths).&#13;
The main concentrations of landslides are on&#13;
moderate-to-steep hillslopes underlain by&#13;
diverse geologic units. For the purpose of&#13;
describing the mapped landslides, we divided&#13;
the study area into five distinct regions&#13;
based on differing geologic and geomorphic&#13;
characteristics. These regions include the&#13;
upper Polochic valley and surrounding highlands,&#13;
the central Sierra de las Minas, the&#13;
hills surrounding La Union and Zacapa, the&#13;
eastern Sierra de las Minas, and the border&#13;
region with Honduras. All of these areas&#13;
received between 200 mm and 600 mm of&#13;
rain over a 13-day period between October&#13;
25 and November 6. The highest rainfall&#13;
amounts (400 mm to 600 mm) occurred in&#13;
the Upper Polochic valley and surrounding&#13;
highlands and in the central Sierra de las&#13;
Minas. The lower rainfall amounts (200 mm&#13;
to 400 mm) occurred in the hills surrounding&#13;
La Union, the eastern Sierra de las&#13;
Minas, and in the border region with&#13;
Honduras. In general, the rainfall received in&#13;
these areas is roughly equivalent to the average&#13;
precipitation received in a 1-year period.&#13;
We used 10-m digital elevation models&#13;
(DEMs) generated from contours on two&#13;
quadrangles in the central Sierra de las&#13;
Minas to create a map showing areas that&#13;
were susceptible to landslides during&#13;
Hurricane Mitch. To create the Hurricane&#13;
Mitch susceptibility map, we developed a&#13;
susceptibility threshold equation based on&#13;
elevation and gradient. The analysis indicates&#13;
that, at least on two quadrangles, gradients&#13;
less than 9? were not susceptible to&#13;
landslides during Hurricane Mitch. The&#13;
slope of the line defined by the threshold&#13;
equation indicates that less rainfall was&#13;
required to initiate landslides on steep gradients&#13;
than on shallow gradients. Ninety percent&#13;
of the mapped landslides that were triggered&#13;
by Hurricane Mitch are within the&#13;
susceptible zone shown on the map. Eightysix&#13;
percent of landslides that were mapped&#13;
as predating Hurricane Mitch, and all landslides&#13;
mapped as postdating Hurricane&#13;
Mitch, are within the susceptible zone.&#13;
We used LAHARZ software to model the&#13;
potential downstream area affected by debris&#13;
if a large landslide dam on the Rio La Lima&#13;
were to fail. The model shows that the area&#13;
affected would be similar to the area that&#13;
was affected by a debris flow that mobilized&#13;
from a large landslide along the Rio La&#13;
Lima during Hurricane Mitch.&#13;
The characteristics of rainfall-triggered&#13;
landslides described in this report can be&#13;
used as a partial guide to future landslide&#13;
activity triggered by rainstorms. On the&#13;
basis of existing data, hazardous areas&#13;
include: moderate to steep hillslopes and&#13;
</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr01443</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Landslides triggered by Hurricane Mitch in Guatemala -- inventory and discussion</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>