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The 2004 and later volcanic activity of Mount St. Helens has been documented as a continuous eruption with a gradual extrusion of magma at the Mount St. Helens volcano in Washington, United States. Since October 2004, there has been a gradual building of a new lava dome. The new dome has not yet risen above the caldera created by the 1980 eruption of Mount St. Helens but is expected to eventually, if the current eruption continues.

On September 23, 2004, around 2:00 a.m. PDT, Mount St. Helens experienced an earthquake swarm, with about 200 small (less than magnitude 1) earthquakes occurring less than one-half mile (one kilometer) below the lava dome. Activity increased, and on September 26, the U.S. Geological Survey (USGS) and Pacific Northwest Seismograph Network issued a "notice of volcanic unrest", stating that a "hazardous event" was possible, and the U.S. Forest Service closed the mountain to all climbing. They also closed some trails in the area because of the risk of debris flows from the possible melting of the Crater Glacier in the volcanic crater.

Seismic activity continued accelerating following the USGS advisory, with earthquakes approaching magnitude 2.5 occurring at a rate of about four per minute on September 29, prompting the USGS and Pacific Northwest Seismograph Network to issue a second advisory, increasing the "alert level" to the second of three levels and warning of an increased likelihood of steam explosion or eruption from the lava dome within the next few days. Such an event was expected to be relatively small and not pose a threat beyond the immediate area of the mountain. However, the earthquake intensities and occurrences continued to rise. In the near vicinity to the volcano, earthquakes were felt as much as four in one minute. The largest earthquake recorded was a magnitude 3.3.

Mt. St. Helens sent a plume of volcanic ash and steam to 10,000 feet (3,000 m) above sea level in its October 1 eruption seen here.

At 12:02 p.m. PDT on October 1, 2004, the mountain threw a plume of steam and volcanic ash about 9,700 feet (about 3 kilometers) into the air (according to pilot reports), from a vent in the unnamed glacier just southwest of the lava dome. The resulting ash plume was reported to have drifted south to Vancouver, Washington, and Wood Village, Oregon, dusting cars with a fine layer of black, sooty ash.

After releasing a cloud of steam on October 2, dust from landslides inside the crater could be observed for the rest of the afternoon.

Mount St. Helens vented another burst of steam the next day at 12:14 p.m. PDT, which was stronger than Friday's steam release. A low-frequency harmonic tremor followed the steam release, which led seismologists to raise the "alert level" to the third of three levels, indicating a potential threat to life and property. Accordingly, the Johnston Ridge Observatory overlooking Mount St. Helens was evacuated; television media established their bases at Castle Lake Viewpoint about nine miles (14 km) away, while tourists moved to various locations for several miles along Washington State Route 504.

On October 3 there was low-frequency harmonic tremor activity begin at around 3:00 a.m. PDT and lasting for up to 90 minutes, which may have indicated the movement of magma beneath the mountain. The tremors were followed by a steam release at around 10:40 a.m.

October 5: Steam and ash eruption, seen from the Johnston Ridge Observatory.

Mount St. Helens eruptive activity continued over the following days, with steam releases occurring on October 4 at 9:47 a.m., 2:12 p.m., and at 5:40 p.m.; then again on the morning of October 5 at around 9:03 a.m., with an ash plume that dusted Randle, Morton, and Packwood, Washington, towns on or near U.S. Highway 12 about 30 miles (48 km) from the volcano. Between steam releases, elevated seismic activity on the mountain continued with the strongest tremors remaining near magnitude 3.0.

On October 6, the U.S. Geological Survey announced that the alert level was being lowered, saying "We no longer think that an eruption is imminent in the sense of minutes or hours."

A steam plume rises from the mountain in December 2004

Magma reached the surface of the volcano around October 11, resulting in the building of a new lava dome on the existing dome's south side. Dome building continued, with the USGS reporting in early November 2004 that magma was extruding onto the surface at a rate of 7 to 10 cubic meters per second. Had magma continued to extrude at this rate uninterrupted, the crater would have been completely filled and Mount St. Helens regained its former height in about eleven years. The new dome became visible behind and to the right of the old dome, when viewed from the Johnston Ridge Observatory. The Mount St. Helens VolcanoCam located at Johnston Ridge is able to view the new dome especially at night when the glow of new magma is visible via the camera's infrared capabilities.

'Whaleback' feature on February 22, 2005.

Included in the new dome was a feature dubbed the "whaleback" (named such because of its close resemblance to the back of a whale), which was a long shaft of solidified magma being exuded by pressure of magma underneath it. This feature was very hot but fragile. The edges of it began crumbling rapidly, forming loose material around the new dome. The rate of crumbling soon matched the rate of growth, with the size of the whaleback remaining fairly constant.

On February 1, 2005, the new lava dome on Mount Saint Helens measured 7,642 feet (2,329 m) in elevation. This brought its elevation to 1,363 feet (415 m) above the 1980 crater floor, approximately 2,000 feet (610 m) above the surface of the Crater Glacier, and 721 feet (220 m) below the highest point of the volcano. The whaleback feature measured approximately 1,550 feet (470 m) in length and 500 feet (150 meters) in width. The diameter of the new dome was about 1,700 feet (520 m), and it contained about 50 million cubic yards (40 million cubic meters) of material. The total amount of glacier lost by this date was estimated to be 5-10%, but the flow of water from the crater was almost unchanged because the porous nature of the floor of the crater caused the water to be absorbed quickly.

March 8, 2005 Eruption

Mount St. Helens had major activity again on March 8, 2005 at about 5:30 p.m. local time, when a 36,000-foot (11 km) plume of steam and presumably ash was witnessed emerging from the volcano, accompanied by a tremor that measured about magnitude 2.5. The plume was visible from the metropolitan areas of Seattle, Washington, to Salem, Oregon, but only lasted for about 20-30 minutes. Ash was reported falling from the sky in Yakima, Washington, and surrounding areas. This activity was not considered a large eruption like those that may still be possible but merely a minor release of pressure consistent with the nature of ongoing dome building. Scientists think it was triggered by a partial collapse of the lava dome. There was no increase in quake activity before the volcanic event.

New dome on May 25, 2005.

As of May 5, 2005, the highest point on the new dome was 7,675 feet (2,339 m), 688 feet (210 meters) below the highest point of the volcano. It contained approximately 58 million cubic yards (45 million cubic meters) of material. Growth of the new dome continues steadily and has not abated, and small earthquakes continue to be observed every few minutes. The whaleback feature is disintegrating steadily but continues to be extruded as solidified lava pushes upward from underneath it. If the growth of the new dome continues at its current pace, the new dome could replace the amount of material lost in the 1980 eruption (estimated at 3.7 billion cubic yards, or 2.8 cubic kilometers) within the next 40-50 years.

On July 2, 2005, the tip of the whaleback feature broke off, causing a rockfall that sent ash and dust several hundred meters into the air. [1]

Scientists closely monitoring the volcano have scaled back their predictions of a bigger eruption. Some are now saying that Mt. St. Helens could continue to experience volcanic events similar to what the mountain had in early October for years to come, without ever causing a major, dramatic eruption.

Following the collapse of the dome and whaleback, a new feature began growing out termed the "slab". Approximately the size of a football field, the large, cooled volcanic rock was being forced upward as quickly as 6 feet (2 m) per day. [2][3]

On July 21, 2006, the rim was reopened to summit hikes[4].

On December 19, an eruption sent a steam plume billowing over Washington.[5]

• 1980 eruption of Mount St. Helens

• Mount St. Helens National Volcanic Monument website from the U.S. Forest Service
• Mount St. Helens National Volcanic Monument's VolcanoCam
• Mt. St. Helens webcam and current time lapse videos
• Mount St. Helens photographs and current conditions from the United States Geological Survey website