April 29, 2010
A weekly feature provided by scientists at the Hawaiian Volcano Observatory.
A Peculiar Flow from Sulphur Cone along Mauna Loa's Southwest Rift Zone
Volcano Watchers may pride themselves on having witnessed a variety of lava flows, but how many can say they've seen flowing molten sulfur? It happens at some volcanoes, including a rare occurrence perhaps 60 years ago at Sulphur Cone on Mauna Loa's southwest rift zone.
Let's first dispel any thought that sulfur flows are like the extensive pāhoehoe and 'a'ā erupted along Kīlauea's east rift zone. Sulfur flows are small, ranging in area from one-tenth to a few hundred square meters (the area of a bandana to the area of a basketball court). And sulfur flows are thin, only a few centimeters (inches) or, rarely, tens of centimeters (a foot or so) thick. But, like many liquids, molten sulfur possesses sufficient viscosity, or resistance to flowage, that it may form features similar to pāhoehoe, such as ridges, toes, channels, levees, and lava tubes.
Another thing to clarify is the origin of the material in a sulfur flow. Molten or partially molten rock within the earth is generated at high temperature and pressure. However, neither condition is necessary to generate a sulfur flow. Sulfur has a low melting temperature, about 112 degrees Celsius (234 degrees Fahrenheit), slightly above the boiling point of water. The earth's surface reaches such a temperature near volcanic fissures or close to active vents, as shown by the areas of steaming ground often observed near hot volcanic features. So all that's needed is a way to deposit sulfur and have it ready for melting when ground temperatures spike.
The depositional volcanic agent is the gas discharged from fumaroles, or gas-emitting vents, which are common on active volcanoes. A familiar example for Kīlauea visitors is Sulphur Bank in Hawai`i Volcanoes National Park. There the bright-yellow crystalline sulfur forms in two ways: by condensation of vaporous sulfur and also by a chemical reaction between sulfur-containing gases. Although molten sulfur droplets have been observed at Sulphur Bank, the sulfur deposits and temperature are insufficient to form an actual sulfur flow.
So we turn to Sulphur Cone, a cinder-and-spatter cone situated on the southwest rift zone of Mauna Loa at an altitude of about 3,430 m (11,240 ft). When named in 1921, the cone was notable for the abundance of sulfur crystals blanketing it and the surrounding area, a consequence of extensive degassing from a fissure downslope from Mauna Loa's summit. This bloom of sulfur at the surface surely marked a subterranean setting where sulfur had crystallized in the voids and coated many fractures. No sulfur flows were recognized in the area when the cone was named in 1921, suggesting that the sulfur flow must be younger than that.
What could have melted all that sulfur to make a flow? One proposed mechanism is that heating along the 20-km-long (12-mile-long) fissure of Mauna Loa's spectacular 1950 eruption substantially raised the ground temperature. Once the temperature exceeded the 112-degree melting point, the accumulated sulfur could melt and issue from cracks—in this case, forming a flow ranging in thickness from 10 to 50 cm (4-20 in.), covering about 380 square meters (450 square yards).
Worth noting is a feature of sulfur flows, recently rediscovered, that was first described in the 1780s at the island of Vulcano, near Sicily (Italy). Molten sulfur, if hot enough, can ignite and burn as it flows. When it does, much of the evidence of its passage may go up in smoke, so to speak; the only remaining trace may be a track of sulfur blocks too large to be entirely consumed.
Thus, sulfur flows are truly anomalous. Typical molten lava flows and ejected spatter glow incandescently, but they don't ignite and burn, despite the vision conveyed by popular terms, such as "fire fountain" or "curtain of fire." Sulfur is a rare instance in our volcanic world where the fire of Dante's Inferno does indeed play upon the surface of a molten flow.
Kīlauea Activity Update
Over the past week, breakouts traveling along the east margin of the Thanksgiving Eve Breakout (TEB) flow on Kilauea's east rift zone continued their journey to the ocean. As of this writing (Thursday, April 29), the active flow front has moved past the end of the Kalapana access road and the County viewing area, creeping through thick vegetation, and triggering small brush fires and minor methane bursts, before entering the ocean at 12:15 p.m. on April 29.
At Kīlauea's summit, a ponded, circulating lava surface deep in the collapse pit within the floor of Halema`uma`u Crater was visible via Webcam during much of the past week. A small collapse of a portion of the vent floor on Monday increased the diameter of the lava pond. Volcanic gas emissions remain elevated, resulting in high concentrations of sulfur dioxide downwind.
One earthquake beneath Hawai`i Island was reported felt during the past week. A magnitude-2.5 earthquake occurred at 3:30 p.m. on Thursday, April 22, 2010, H.s.t., and was located 9 km (6 miles) west of Waikoloa Village, at a depth of 11 km (7 miles).
Visit our Web site (http://hvo.wr.usgs.gov) for detailed Kīlauea and Mauna Loa activity updates, recent volcano photos, recent earthquakes, and more; call (808) 967-8862 for a Kīlauea activity summary; email questions to askHVO@usgs.gov.
Updated: May 28, 2010 (pnf)