Thursday, May 19, 2005
A walk down memory lane
The eruption was preceded by a two-month long series of earthquakes and steam venting episodes, caused by an injection of magma at shallow depth below the mountain which created a huge bulge and a fracture system on Mount St. Helens' north slope. An earthquake on May 18, 1980, caused the entire weakened north face to slide away, suddenly exposing the partly molten, gas- and steam-rich rock in the volcano to lower pressure.
The rock responded by exploding into a super-heated mix of pulverized lava and older rock that sped toward Spirit Lake so fast that it quickly passed the avalanching north face. A volcanic ash column rose high into the atmosphere and deposited ash in eleven U.S. States. At the same time, snow, ice, and several entire glaciers on the mountain melted, forming a series of large lahars (volcanic mudslides) that reached as far as the Columbia River.
Less severe outbursts continued into the next day only to be followed by other large but not as destructive eruptions later in 1980. By the time the ash settled, 57 people (including innkeeper Harry Truman and geologist David A. Johnston) and thousands of animals were dead, hundreds of square miles (mi²) reduced to wasteland, over a billion U.S. dollars in damage had occurred, and the once graceful face of Mount St. Helens was scarred with a huge crater open to the north.
The area was later preserved, as it was, in the Mount St. Helens National Volcanic Monument. Several small earthquakes beginning as early as March 16, 1980, indicated that magma may have been moving below the volcano. Then on March 20 at 3:47 PM Pacific Standard Time (all times will be in PST), a shallow Richter magnitude 4.2 earthquake, centered below the mountain's north flank, definitely signaled the volcano's violent return from 123 years of hibernation.
A gradually building earthquake swarm saturated area seismographs and started to climax at about noon on March 25, reaching peak levels in the next two days (a total of 174 shocks of 2.6 or greater were recorded during those two days). Shocks of 3.2 or greater occurred at a slightly increasing rate through April and May with five earthquakes of magnitude 4 or above per day in early April, and 8 per day the week before May 18. Initially there was no direct sign of eruption, but small earthquake-induced avalanches of snow and ice were reported from aerial observations.
Then at 12:36 PM on March 27, at least one but possibly two nearly simultaneous phreatic eruptions (exploding groundwater-derived steam) ejected pulverized rock from within the old summit crater, excavating a new crater 250 feet (76 m) wide and sending an ash column about 6,000 feet (1800 m) into the air. Also by this date, a 16,000 foot (4900 m) long east-trending fracture system had developed across the summit area.
This was followed by more earthquake storms and a series of steam explosions that sent ash 10,000 to 11,000 feet (3050 to 3350 m) above their vent. Most of this ash fell within 3 to 12 miles (5 to 19 km) from its vent but some was carried as far as 150 miles (240 km) south to Bend, Oregon, and 285 miles (459 km) east to Spokane, Washington. A second new crater and a blue flame were observed on March 29. The flame danced to and from the two craters and was probably created by burning gases.
Static electricity generated from ash clouds rolling down the mountain sent out lightning bolts that were up to two miles (3 km) long. 93 separate outbursts were reported on March 30, and harmonic tremors were detected on April 3, alarming geologists and prompting the governor to declare a state of emergency. By April 8 the two craters merged, eventually creating one that was 1,700 to 850 feet (520 to 260 m) wide.
A USGS team determined in the last week of April that a 1.5 mile (2.4 km) diameter section of St. Helens' north face was displaced out at least 270 feet (82 m). For the rest of April and early May this bulge grew 5 to 6 feet per day (1.5 to 1.8 m), and by mid-May it extended more than 400 feet (120 m) north. As the bulge moved northward, the summit area behind it progressively sank, forming a complex down-dropped block called a graben.
Geologists announced on April 30 that sliding of the bulge area was the greatest immediate danger and that such a landslide may spark an eruption. These changes in the volcano's shape were related to the overall deformation that increased the volume of the mountain by 0.03 cubic mile (125,000,000 m³) by mid-May. This volume increase presumably corresponded to the volume of magma that pushed into the volcano and deformed its surface.
Because the intruded magma remained below ground and was not directly visible, it was called a cryptodome, in contrast to a true volcanic dome exposed at the surface. On May 7, eruptions similar to those in March and April resumed, and over the next several days the bulge grew to huge proportions. All activity to this point was confined to the 350-year-old summit dome and did not involve any new magma.
A total of about 10,000 earthquakes were recorded prior to the May 18th event with most concentrated in a small zone less than 1.6 miles (2.6 km) directly below the bulge. Visible eruptions then ceased on May 16, reducing public interest and consequently the number of spectators in the area. Mounting public pressure then forced officials to allow a limited number of people to enter the danger zone on May 17 to gather whatever property they could carry.
Another trip was scheduled for 10 AM the next morning. Since that was Sunday, more than 300 loggers would not be working in the area. By the time of the climactic eruption, an estimated 0.11 cubic kilometers of dacite magma had intruded into the volcano. The rising magma forced the volcano's north flank outward nearly 500 feet (150 m) and heated the volcano's ground water system, causing many steam-driven explosions (phreatic eruptions).
At 7 AM on May 18, USGS volcanologist David A. Johnston, who had Saturday night duty at an observation post about 6 miles (10 km) north of the mountain, radioed in the results of some laser-beam measurements he had made moments earlier. Mount St. Helens' activity that day did not show any change from the pattern of the preceding month. The rate of bulge movement, sulfur-dioxide gas emission, and ground temperature readings did not reveal any unusual changes that might indicate a catastrophic eruption.
Without warning at 8:32 AM, a magnitude 5.1 earthquake (seismograph) centered directly below the north slope triggered that part of the mountain to slide an estimated 7–20 seconds (about 10 seconds seems most reasonable) after the shock. One of the largest landslides in recorded history, the slide traveled at 110 to 155 miles per hour (175 to 250 km/h) and moved across Spirit Lake's west arm; part of it hit a 1,150 foot (350 m) high ridge about 6 miles (9.5 km) north.
Some of the slide spilled over the ridge, but most of it moved 13 miles (21 km) down the North Fork Toutle River, filling its valley up to 600 feet (180 m) deep with avalanche debris. An area of about 24 mile² (62 km²) was covered, and the total volume of the deposit was about 0.7 mile³ (2.9 km³). Most of St. Helens' former north side became a rubble deposit 17 miles (27 km) long, averaging 150 feet (46 m) thick; the slide was thicker a mile (1.6 km) below Spirit Lake and thinnest at its western margin.
All the water in Spirit Lake was temporarily displaced by the landslide, sending 600 foot (180 m) high waves crashing into a ridge north of the lake and adding 295 feet (90 m) of new avalanche debris above the old lakebed, raising its surface level by about 200 feet (60 m). As the water moved back into its basin, it pulled thousands of trees felled by a super-heated wall of volcanic gas and searing ash and rock that overtook the landslide seconds before (see below).
The landslide suddenly exposed the dacite magma in St. Helens' neck to much lower pressure, causing the gas-charged, partially molten rock and high-pressure steam above it to explode a few seconds after the slide started. Explosions burst through the trailing part of the landslide, blasting rock debris northward. The resulting laterally-directed pyroclastic flow of super-heated volcanic gases, ash and pumice from new lava, and pulverized old rock hugged the ground while initially moving at 220 mph (350 km/h) but quickly accelerating to 670 mph (1080 km/h) (it may have briefly passed the speed of sound).
Pyroclastic flow material passed up the moving avalanche and spread outward, devastating a fan-shaped area 23 miles (37 km) across and 19 miles (30 km) long. In all, about 230 square miles (600 km²) of forest were knocked down within an 8 mile (13 km) inner fan area, and extreme heat killed trees miles beyond the blow-down zone. At its vent the lateral blast probably did not last longer than about 30 seconds, but the northward radiating and expanding blast cloud continued for about another minute.
Super-heated flow material flashed water in Spirit Lake and North Fork Toutle River to steam, creating a larger secondary explosion that was heard as far away as British Columbia, Montana, Idaho, and Northern California. Yet many areas closer to the eruption (Portland, Oregon, for example) did not hear the blast. This so-called "quiet zone" extended radially a few tens of miles from the volcano and was created due to the complex response of the eruption's sound waves to differences in temperature and air motion of the atmospheric layers and, to a lesser extent, local topography.
Everyone in the quiet zone did see the resulting huge ash cloud that was sent skyward from St. Helens' northern foot. The near-supersonic lateral blast, loaded with volcanic debris, caused widespread devastation as far as 19 miles (30 km) from the volcano. The area affected by the blast can be subdivided into three roughly concentric zones: Direct blast zone, the innermost zone, averaged about 8 miles (13 km) in radius, an area in which virtually everything, natural or artificial, was obliterated or carried away.
For this reason, this zone also has been called the "tree-removal zone." The flow of the material carried by the blast was not deflected by topographic features in this zone. Channelized blast zone, an intermediate zone, extended out to distances as far as 19 miles (30 km) from the volcano, an area in which the flow flattened everything in its path and was channeled to some extent by topography. In this zone, the force and direction of the blast are strikingly demonstrated by the parallel alignment of toppled large trees, broken off at the base of the trunk as if they were blades of grass mown by a scythe.
This zone was also known as the "tree-down zone." Seared zone, also called the "standing dead" zone, the outermost fringe of the impacted area, a zone in which trees remained standing but were singed brown by the hot gases of the blast. Later studies indicated that one third of the 0.045 cubic miles (188,000,000 m³) of material in the flow was new lava, and the rest was fragmented older rock.
By the time this pyroclastic flow hit its first human victims, it was still as much as 680°F (360°C) and filled with suffocating gas and flying angular material. Most of the 57 people known to have died in that day's eruption succumbed to suffocation while several died from burns. Lodge owner Harry Truman was buried under hundreds of feet (tens of metres) of avalanche material. Volcanologist David A.
Johnston was one of those killed, as was Reid Blackburn, a National Geographic photographer. Subsequent outpourings of pyroclastic material from the breach left by the landslide consisted mainly of new magmatic debris rather than fragments of preexisting volcanic rocks. The resulting deposits formed a fan-like pattern of overlapping sheets, tongues, and lobes. At least 17 separate pyroclastic flows occurred during the May 18 eruption, and their aggregate volume was about 0.05 mile³ (208,000,000 m³).
The flow deposits were still about 570°F to 785°F (300°C to 420°C) two weeks after they erupted. Secondary steam-blast eruptions fed by this heat created pits on the northern margin of the pyroclastic flow deposits, at the south shore of Spirit Lake, and along the upper part of the North Fork Toutle River. These steam-blast explosions continued sporadically for weeks or months after the emplacement of pyroclastic flows, and at least one occurred about a year later, on May 16, 1981.
As the avalanche and initial pyroclastic flow were still advancing, a huge ash column grew to a height of 12 miles (19 km) above the expanding crater in less than 10 minutes and spewed tephra into the stratosphere for 10 straight hours. Near the volcano, the swirling ash particles in the atmosphere generated lightning, which in turn started many forest fires. During this time, parts of the now mushroom-shaped ash cloud column collapsed, sending additional pyroclastic flows speeding down St. Helens' flanks.
Later, slower flows came directly from the new north-facing crater and consisted of glowing pumice bombs and very hot pumiceous ash. Some of these hot flows covered ice or water which flashed to steam, creating craters up to 65 feet (20 m) in diameter and sending ash as much as 6,500 feet (1980 m) into the air. Strong high-altitude wind carried much of this material east-northeastly from the volcano at an average speed of about 60 mph (100 km/h).
By 9:45 AM it had reached Yakima, Washington, 90 miles (145 km) away, and by 11:45 AM it was over Spokane, Washington. A total of 4 to 5 inches (100 to 130 mm) of ash fell on Yakima, and areas as far east as Spokane were plunged into darkness by noon where visibility was reduced to 10 feet (3 m) and half an inch (10 mm) of ash fell. Continuing east, St. Helens' ash fell in the western part of Yellowstone National Park by 10:15 PM and was seen on the ground in Denver, Colorado, the next day.
In time ashfall from this eruption was reported as far away as Minnesota and Oklahoma, and some of the ash drifted around the globe within about 2 weeks. During the 9 hours of vigorous eruptive activity, about 540 million tons of ash fell over an area of more than 22,000 mile² (60,000 km²). The total volume of the ash before its compaction by rainfall was about 0.3 mile³ (1.3 km³). The volume of the uncompacted ash is equivalent to about 0.05 mile³ (208,000,000 m³) of solid rock, or only about 7 percent of the amount of material that slid off in the debris avalanche.
By around 5:30 PM on May 18, the vertical ash column declined in stature, but less severe outbursts continued through the night and the following several days. The hot, exploding material also broke apart and melted nearly all of the mountain's glaciers along with most of the overlying snow. As in many previous St. Helens eruptions, this created huge lahars (volcanic mudslides) and muddy floods that affected 3 of the 4 stream drainage systems on the mountain and which started to move as early as 8:50 AM.
Lahars traveled as fast as 90 mph (145 km/h) while still high on the volcano but progressively slowed to about 3 mph (5 km/h) on the flatter and wider parts of rivers. Mudslides off the southern and eastern flanks had the consistency of wet concrete as they raced down Muddy River, Pine Creek, and Smith Creek to their confluence at the Lewis River. Bridges were taken out at the mouth of Pine Creek and the head of Swift Reservoir, which rose 2.6 feet (0.8 m) by noon to accommodate the nearly 18 million yard³ (13 million m³) of additional water, mud, and debris.
Glacier and snow melt mixed with tephra on the volcano's northeast slope to create much larger lahars. These mudslides traveled down the north and south forks of the Toutle River and joined at the confluence of the Toutle forks and the Cowlitz River near Castle Rock, Washington, at 1:00 PM. Ninety minutes after the eruption, the first mudflow had moved 27 river miles (43 km) upstream where observers at Weyerhauser's Camp saw a 12 foot (3.7 m) high wall of muddy water and debris pass.
Near the confluence of the Toutle's north and south forks at Silver Lake, a record flood stage of 23.5 feet (7.16 m) was recorded. A large but slower moving mudflow with a mortar-like consistency was mobilized in early afternoon at the head of North Fork Toutle. By 2:30 PM the massive mudflow had destroyed Weyerhauser's Camp Baker, and in the following hours seven bridges were carried away.
Part of the flow backed up for 2.5 miles (4 km) soon after entering the Cowlitz River but most continued downstream. After traveling 17 miles (27 km) more, an estimated 3.9 million yard³ (2.98 million m³) of material were injected into the Columbia River, reducing the river's depth by 25 feet (7.6 m) for a four mile (6 km) stretch.
The resulting 13 foot (4 m) river depth temporarily closed the busy channel to ocean-going freighters, costing Portland, Oregon, an estimated five million US dollars. Ultimately more than 65 million yard³ (50 million m³) of sediment were dumped along the lower Cowlitz and Columbia Rivers. The May 18, 1980, event was the most deadly and economically destructive volcanic eruption in the history of the United States.
Fifty-seven people were killed and 200 homes, 47 bridges, 15 miles (24 km) of railways and 185 miles (300 km) of highway were destroyed. U.S. President Jimmy Carter surveyed the damage and stated it looked more desolate than a moonscape. A film crew was dropped by helicopter on St. Helens on May 23 to document the destruction.
Their compasses, however, spun in circles and they quickly became lost. A second eruption occurred the next day (see below), but the crew survived and was rescued two days after that. In all, St. Helens released an amount of energy equivalent to 27,000 Hiroshima-sized atomic bombs and ejected more than 1 cubic mile (4 km³) of material. One fourth of that volume was fresh lava in the form of ash, pumice, and volcanic bombs while the rest was fragmented older rock.
The removal of the north side of the mountain reduced St. Helens' height by about 1,313 feet (400 m) and left a crater 1 to 2 miles (2 to 3 km) wide and 2,100 feet (640 m) deep with its north end open in a huge breach. More than 4 billion board feet (14.6 km³) of timber were damaged or destroyed, primarily by the lateral blast. At least 25 percent of the destroyed timber was salvaged after September 1980.
Downwind of the volcano, in areas of thick ash accumulation, many agricultural crops, such as wheat, apples, potatoes, and alfalfa, were destroyed. 1,500 elk and 5,000 deer were killed, and an estimated 12 million Chinook and Coho Salmon fingerlings died when their hatcheries were destroyed. Another estimated 40,000 young salmon were lost when they swam through turbine blades of hydroelectric generators due to the need to have low reservoirs levels along the Lewis River to accommodate possible mudflows and flood waters.
The ash fall created some temporary but major problems with transportation, sewage disposal, and water treatment systems. Visibility was greatly decreased during the ash fall, closing many highways and roads. Interstate 90 from Seattle to Spokane was closed for a week. Air transportation was disrupted for a few days to 2 weeks as several airports in eastern Washington shut down due to ash accumulation and poor visibility.
Over a thousand commercial flights were canceled following airport closures. Fine-grained, gritty ash caused substantial problems for internal-combustion engines and other mechanical and electrical equipment. The ash contaminated oil systems, clogged air filters, and scratched moving surfaces. Fine ash caused short circuits in electrical transformers, which in turn caused power blackouts. Removing and disposing of the ash was a monumental task for some eastern Washington communities.
State and Federal agencies estimated that over 2.4 million yard³ (1.8 million m³) of ash—equivalent to about 900,000 tons in weight—were removed from highways and airports in Washington. Ash removal cost $2.2 million and took 10 weeks in Yakima. The need to remove ash quickly from transportation routes and civil works dictated the selection of some disposal sites.
Some cities used old quarries and existing sanitary landfills; others created dumpsites wherever expedient. To minimize wind reworking of ash dumps, the surfaces of some disposal sites have been covered with topsoil and seeded with grass. Early estimates of the cost of the eruption ranged from US $2–3 billion. A refined estimate of $1.1 billion was determined in a study by the International Trade Commission at the request of the United States Congress.
A supplemental appropriation of $951 million for disaster relief was voted by Congress, of which the largest share went to the Small Business Administration, U.S. Army Corps of Engineers, and the Federal Emergency Management Agency. There were also indirect and intangible costs of the eruption. Unemployment in the immediate region of Mount St. Helens rose tenfold in the weeks immediately following the eruption and then nearly returned to normal once timber salvaging and ash-cleanup operations were underway.
Only a small percentage of residents left the region because of lost jobs owing to the eruption. Several months after May 18, a few residents reported suffering stress and emotional problems, even though they had coped successfully during the crisis. Counties in the region requested funding for mental health programs to assist such people. Initial public reaction to the May 18 eruption nearly dealt a crippling blow to tourism, an important industry in Washington.
Not only was tourism down in the Mount St. Helens–Gifford Pinchot National Forest area, but conventions, meetings, and social gatherings also were canceled or postponed at cities and resorts elsewhere in Washington and neighboring Oregon not affected by the eruption. The negative impact on tourism and conventioneering, however, proved only temporary. Mount St. Helens, perhaps because of its reawakening, has regained its appeal for tourists.
The National Forest Service and the State of Washington opened visitor centers and provided access for people to view the volcano's devastation. St. Helens produced five more explosive eruptions in the summer and fall of 1980. Through early 1990, a total of at least 21 periods of eruptive activity had occurred. An eruption occurred on May 25 at 2:30 AM that sent an ash column 9 miles (14 km) into the atmosphere. The eruption was preceded by a sudden increase in earthquake activity and occurred during a rain storm.
Erratic wind from the storm carried ash from the eruption to the south and west, lightly dusting large parts of western Washington and Oregon. Pyroclastic flows exited the northern breach and covered avalanche debris, lahars, and other pyroclastic flows deposited by the May 18 eruption. At 7:05 PM on June 12, a plume of ash billowed 2.5 miles (4 km) above the volcano. At 9:09 PM a much stronger explosion sent an ash column about 10 miles (16 km) into the air.
A dacite dome then oozed into existence on the crater floor, growing to a height of 200 feet (60 m) and a width of 1,200 feet (365 m) inside a week. A series of large explosions on July 22 broke more than a month of relative quiet. The July eruptive episode was preceded by several days of measurable expansion of the summit area, heightened earthquake activity, and changed emission rates of sulfur dioxide and carbon dioxide. The first hit at 5:14 PM as an ash column shot 10 miles (16 km) and was followed by a faster blast at 6:25 PM that pushed the ash column above its previous maximum height in just 7.5 minutes.
The final explosion started at 7:01 PM and continued for over two hours. When the relatively small amount of ash settled over eastern Washington, the dome built in June was gone. Seismic activity and gas emission steadily increased in early August, and on August 7 at 4:26 PM, an ash cloud slowly expanded 8 miles (13 km) skyward. Small pyroclastic flows were sent through the northern breach and weaker outpouring of ash rose from the crater. This continued until 10:32 PM when a second large blast sent ash high into the air.
A second dacite dome filled this vent a few days later. Two months of repose were ended by an eruption lasting from October 16 to October 18. This event obliterated the second dome, sent ash 10 miles (16 km) in the air and created small, red-hot pyroclastic flows. A third dome began to form within 30 minutes after the final explosion on October 18, and within a few days, it was about 900 feet (275 m) wide and 130 feet (40 m) high. All of the post-1980 eruptions were quiet dome-building events, beginning with the December 27, 1980, to January 3, 1981, episode. By 1987 the third dome had grown to be more than 3,000 feet (900 m) wide and 800 feet (240 m) high.
At this rate and assuming additional destructive eruptions do not occur, St. Helens' summit should be restored sometime in the mid to late 22nd century. In September–October 2004, however, St. Helens came back to life, and as of Oct. 2, scientists are anticipating another eruption. See the main Mount St. Helens article for the most recent updates.