Volcano Watch - How do lava flows cool and how long does it take?

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Eruptive lava temperatures of the 2018 LERZ eruption reached a maximum of approximately 1140 degrees Celsius (2080 degrees Fahrenheit). When the entire flow cools below about 1000 degrees Celsius (1800 degrees Fahrenheit), it has solidified, but the interior is still very hot.

Arguably the most influential factor determining how fast lava cools is the thickness of the flow. Other factors include heat loss from both the top (to the atmosphere) and bottom of a flow (into the ground). Contributing to heat loss at the flow's surface are air temperature, rainfall, and wind.

The initial contact between a lava flow, the air above it, and ground surface below it, quickly hardens the outer crust (top and bottom) of the flow. This is apparent in the silvery crust that forms on active pāhoehoe flows and the rubbly clinker that surrounds active ‘a‘ā flows. As the crust cools and thickens, it retains heat within the flow's interior. This is because the crust is a good insulator, meaning it poorly conducts heat—similar to how an insulated thermos keeps liquid inside it hot.

After the initial formation of crust, the flow continues to lose heat through radiation and conduction, facilitated by wind and rain. As rain water percolates into cracks in the flow's surface and encounters the hot interior, it produces steam, forming the billowy white plumes often seen over active (or recently active) flows. This steaming can persist for decades, long after the lava has solidified, depending on the thickness of the flow and the temperature of its interior.

Based on a study of crustal cooling of pāhoehoe lava flows in Kalapana erupted from the East Rift Zone Kupaianaha vent in 1990, we can estimate the solidification time for the 2018 LERZ flows. Because the equation only looks at cooling of the lava flow's upper crust, the basal crust thickness is assumed to equal 70 percent of the upper crust according to this study.

The Kalapana measurements were made on thin pāhoehoe flows, but most of the 2018 LERZ lava is ‘a‘ā. However, because the core of each flow type should cool at similar rates, we are basing 2018 cooling rates on the 1990 study. Also, of note, the flows studied in 1990 were much thinner with shorter cooling rates and may not account for long-term changes in wind and rain patterns.

Preliminary analyses of the 2018 LERZ eruption flow thicknesses, suggest that the average flow thickness is around 10–15 m (33–50 ft). Based on the cooling rate calculation, it could take roughly 8 months to 1.5 years for flows of these thicknesses to solidify.

Solidification of flows ranging 20–30 m (65–100 ft) thick could take about 2.5–6 years. The thickest LERZ flows on land, which are approximately 55 m (180 ft) thick, may take roughly 20 years to reach a completely solid state.

Because flow thickness, wind speeds, rainfall amounts, air and ground temperatures, and other factors all affect lava cooling rates, there is a range of uncertainty on how long the interior of a flow remains liquid. For example, after the 1959 Kīlauea Iki eruption, the approximately 135 m (440 ft) deep lava lake took about 35 years to completely solidify, and the interior of the lake could still be hot enough today that the rock is incandescent. This is why, on rainy days, you can see steam rising from the Kīlauea Iki crater floor, as well as the Kīlauea caldera floor.

With flow crust being such an efficient insulator, it can take years to decades for lava within thick flows to solidify. It takes much longer for the flow to cool to ambient temperatures.

Next week's Volcano Watch will address in more detail the thicknesses of lava flows from Kīlauea's 2018 lower East Rift Zone eruption.

Volcano Activity Update

Kīlauea is not erupting. Rates of seismicity, deformation, and gas release have not changed significantly over the past week.

Two earthquakes with three or more felt reports occurred in Hawai‘i during the past week: a magnitude-3.0 quake 7 km (4 mi) south of Leilani Estates at 8 km (5 mi) depth on Feb. 22 at 2:31 a.m. HST, and a magnitude-3.2 quake 17 km (11 mi) southeast of Volcano at 7 km (4 mi) depth on Feb. 21 at 11:32 a.m. HST.

Deformation signals are consistent with refilling of Kīlauea Volcano's deep East Rift Zone (ERZ) magma reservoir. Sulfur dioxide emission rates on the ERZ and at Kīlauea's summit remain low.

Hazardous conditions still exist at both the lower ERZ and summit of Kīlauea. Residents and visitors in the lower Puna District and Kīlauea summit areas on the Island of Hawai‘i should stay informed and heed Hawai‘i County Civil Defense closures, warnings, and messages (http://www.hawaiicounty.gov/active-alerts). HVO continues to closely monitor Kīlauea for any sign of increased activity.

The USGS Volcano Alert level for Mauna Loa remains at NORMAL.