As days get shorter and nights cooler, we look to the summit of majestic Mauna Kea after rainstorms to see whether there might be a cap of pure white snow. As days get shorter and nights cooler, we look to
As days get shorter and nights cooler, we look to the summit of majestic Mauna Kea after rainstorms to see whether there might be a cap of pure white snow.
Not very long ago, in geological terms, the white mantle was ever-present on Mauna Kea. The last of the glacial episodes that Mauna Kea experienced covered the summit in ice and snow from about 40,000 to 13,000 years ago.
The glaciers that flowed from the summit left distinctive features. The most prominent of these are extensive deposits of glacial till — accumulations of jagged boulders, stones, cinder and ash. There is also evidence of eruptions interacting with the glaciers. The lava flows that chilled very quickly against glacial ice produced the especially fine-grained, dense rock that was so prized by ancient Hawaiians for making adzes. The famous Mauna Kea adze quarry complex, covering about 4.6 square miles, is near the summit, just below Lake Waiau.
Lake Waiau, in the Mauna Kea Ice Age Natural Area Reserve, is the only alpine lake in the Hawaiian Islands chain, lying within Puu Waiau at about 13,020 feet elevation. Besides the significant archaeological and geological features, Lake Waiau has cultural and spiritual significance to many Hawaiians.
The lake has been shrinking at a rapid rate during the last year. While fluctuations in lake level have been observed in the past, the recent rate of decline seems to be unusually rapid and severe. Theories about the shallowing are tied into theories about why the lake is there at all.
Studies of the chemical signatures of the lake and geomorphology of the area show that the source of the water is precipitation falling within Puu Waiau, mainly from winter storms. The reason for the ponding of the rainwater and snowmelt is less clear, however.
Several mechanisms have been proposed to explain the impermeable layer that traps the lake water. One suggestion is that sulfur-bearing steam emanating from Puu Waiau either during or just after eruptions altered the cinder and ash to fine clay minerals that reduced permeability.
Another suggestion is that the impermeable layer that traps the lake water is made up of the fine-grained ash beds that are found at Puu Waiau and this ash is a result of Waiau eruptions occurring under glacial ice.
One scenario suggests that permafrost makes up the impervious layer beneath the lake, based on the existence of permafrost at nearby Puu Wekiu. However, temperatures taken in the bottom sediment of the lake down to 230 feet in the winter of 1966 did not fall below freezing — the lowest temperature recorded was about 39 degrees.
What implications do these mechanisms have for the shrinking of Lake Waiau? If the impermeable layer beneath the lake was because of permafrost, then the shallowing of the lake could be a result of the permafrost slowly starting to melt, starting at the edges of the lake where, perhaps, insulating sediment layers are less thick. In this scenario, the lake would surely disappear as the permafrost continues to melt with increasing temperatures on Mauna Kea. The temperature increase is about three times faster than the global rate, and is observed at high elevations throughout Hawaii.
If the lake is retained by clay-rich ash beds, then the most likely reason the lake is shrinking is that the evaporation rate is higher than the precipitation rate. The higher average temperatures, along with recent drought conditions, make this the most plausible scenario.
Through a collaboration between the Department of Land and Natural Resources, the Office of Mauna Kea Management and the University of Hawaii at Hilo, research is under way to monitor lake level changes and to reconstruct past lake levels and climatic conditions. Contact the Office of Mauna Kea Management if you have historical photographs of the lake that you are willing to share.
Although the rising temperatures do not bode well for the future of Lake Waiau, a winter season rich in storms will do much to replenish the lake, as well as provide us with magnificent views of the snow-capped volcano.
Kilauea activity update
A lava lake within the Halemaumau Overlook vent produced nighttime glow visible from the Jaggar Museum overlook and by HVO’s webcam during the past week. The lava level fluctuated slightly because of several deflation-inflation cycles at the summit and several brief gas-driven rise-fall cycles.
On Kilauea’s east rift zone, surface lava flows remain active above the pali, near the top of the abandoned Royal Gardens subdivision, about 3.4 miles southeast of Puu Oo. The lava pond in the northeastern pit in Puu Oo crater was visible in the webcam over the past week, with the level fluctuating slightly because of deflation-inflation cycles. Small amounts of lava were also visible in the southern pit on the crater floor.
One felt earthquake was reported in the last week on the Big Island. A magnitude 3.0 earthquake occurred at 4:23 a.m. Tuesday located 3 miles south of Volcano at a depth of 2 miles.
Visit hvo.wr.usgs.gov for detailed Kilauea, Mauna Loa and Hualalai activity updates, recent volcano photos, recent earthquakes and more; call 967-8862 for a Kilauea summary; email questions to askHVO@usgs.gov.
Volcano Watch is a weekly article and activity update written by scientists at the U.S. Geological Survey’s Hawaiian Volcano Observatory.
