This massive boulder (top photo) was carried down the Biwasawa valley on the east side of Bandai volcano in a mudflow during an eruption in 1888. The mudflow deposit covers the broad floor of the Nagase valley. In addition to this mudflow, the 1888 eruption included a pyroclastic flow on the east side and catastrophic debris avalanche that swept over villages to the north of the volcano. The bottom photo is taken from the same location in 1988. The identical boulder now forms part of the landscaping of a house in the town of Inawashiro. Top photo by Fukushima Minposha Newspaper; bottom photo by Lee Siebert (Smithsonian Institution).
This massive rounded boulder on the SW side of Cotopaxi volcano was carried in a lahar, or volcanic mudflow, possibly during a major eruption in 1877. Scale is provided by volcanologists Minard Hall and Patty Mothes of Ecuador's national university, who have spent many years assessing hazards from Ecuador's volcanoes. More than 130,000 persons live in areas subject to lahar risk from Cotopaxi. The 1877 eruption produced lahars that covered this valley, swept into the Amazon basin, and reached the Pacific Ocean along valleys to the NW.
Volcanic mudflows, also known by their Indonesian name, lahars, are water-saturated mixtures of volcanic debris that sweep down volcanoes and valley floors far beyond. These lahars from the 1982 eruption of Galunggung volcano on the Indonesian island of Java caused extensive damage to houses and croplands. Unlike pyroclastic flows, mudflows are generally low temperature, and these houses were not ignited. Mudflows can remain a hazard long after an eruption ends as heavy rainfall redistributes tephra produced by the eruption.
A massive volcanic mudflow produced by collapse of Mount Hood during the Pleistocene swept down the Hood River valley and traveled across the Columbia River, temporarily damming it to a depth of 30 m. This thick outcrop of the mudflow deposit, containing rounded boulders in a clay-rich matrix, is located north of Underwood, Washington, on the other side of the Columbia River.
A hot lahar sweeps down a channel on the SW flank of Mayon volcano in the Philippines on September 14, 1984, five days after the onset of an eruption. The water temperature of this lahar was about 80 degrees Centigrade. Note the large block in the center of the channel that is being transported by the lahar.
Lahars produced devastating personal and economic disruption for many years after the 1991 eruption of Pinatubo in the Philippines. The towns of Barangay Manibaug Pasig, in the foreground of this February 26, 1994 view, and Mancatian in the distance were progressively buried over a several-year period. Construction of lahar levees provided only temporary protection from the massive downstream redistribution of ash and pumice from the 1991 eruption.
Floodwaters back up over the villages of Aglao and Dalanawan on the SW flank of Pinatubo volcano in the Philippines. Lake Mapanuepe was formed when lahars from the 1991 eruption of Pinatubo eruption traveled down the Marella River and dammed its tributary, the Mapanuepe River. Several villages were submerged by the rising lake waters. The level of the lake was stabilized in late 1992 at about this level by excavation of a trench through bedrock in the background. This prevented catastrophic rapid draining of the lake.
These thin, relatively fine-grained layers are lahar deposits produced by successive overflows of dikes along the Bambam River, about 35 km NE of Pinatubo volcano in the Phillipines. The photo was taken on October 13, 1991, a little more than a month after the end of the devastating 1991 eruption. Note the pen at the upper left for scale. By the end of 1991, rainfall-induced lahars had traveled 50 km down the Bambam River from the volcano.
A lahar, or volcanic mudflow, fills the banks of the Pasig-Potrero River on the east side of Pinatubo volcano in the Philippines on October 13, 1991. The lahar moved at a velocity of 3-5 m/sec, and carried a few meter-sized boulders. This lahar was not directly produced by an eruption, but was triggered by minor rainfall, which remobilized thick deposits of ash and pumice that blanketed the landscape. Devastating mudflows occurred at Pinatubo for years after the catastrophic 1991 eruption.
Lahars from Pinatubo volcano fill the broad Santo Tomás River valley SW of the volcano. Erosion along the south bank of the river has cut into the town of San Rafael. This photo was taken a month after the end of the 1991 eruption. Lahars produced by the redistribution of thick deposits of ashfall and pyroclastic flows caused extensive longterm economic devastation and were expected to continue for as long as a decade after the eruption.
Lahars that formed during the 1989-90 eruptions of Redoubt Volcano in Alaska accumulated in the Drift River Valley NE of the volcano. The largest lahars, such as this one from the February 15, 1990 eruption, covered the valley floor nearly wall-to-wall and extended more than 35 km to the Cook Inlet.
A cluster of rounded boulders was deposited on a river terrace by a lahar in the Rio Chinchina valley, 59 km WNW of the summit of Colombia's Nevado del Ruiz volcano on November 13, 1985. The boulders were carried as bedload and deposited against the tree, which served as an obstruction to flow. Note the mudline on the tree that marks the upper flow surface of the lahar.
Lahar deposits produced by redistribution of material shed off the Santiaguito lava dome, visible below the steam plume to the left of Guatemala's Santa Maria volcano, have had dramatic effects on downstream drainages. This December 1988 photo shows the Rio Tambor, SW of Santa Maria, filled bank-to-bank with debris. Bridges such as the one in the foreground have been frequently destroyed during rainy-season lahars, which have traveled 35 km or more from the volcano.
The twisted girders of a highway bridge lie entombed in mudflow deposits from Mount St. Helens. This May 18, 1980 mudflow was produced by dewatering of the debris-avalanche deposit in the North Fork of the Toutle River and traveled as far as the Columbia River, decreasing the depth of the navigational channel from 11 meters to 4 meters.
A house on the SW flank of Unzen volcano is buried to its eaves by deposits from lahars (volcanic mudflows). Redistribution of material shed off of Fugen-dake lava dome (background) produced lahars that devastated populated areas near the volcano. The lahars had low temperatures, unlike pyroclastic flows, and did not ignite the houses. Dome growth, which had begun in May 1991, ceased at about the time of this February 3, 1995 photo.