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View of the recently erased boiling pots on the Willow River in Hilo. The pots, about 15 meters (50 feet) in diameter, corrode to the 10,000-year-old Mauna Loa lava flow. When the water is low, the river does not flow over some edges of the bowl but continues to flow through it. USGS photos.

Hawaiian Subaba Man, Demai Maoist, has made several adventures on the Willow River in the mythical past. He saved his mother, Hina, who lived in the cave behind Wayano (Rainbow Falls), from Kona, a threatened Muyo (legendary giant lizard), eventually killing him and leaving his body as a small island in the pool opposite Hina’s cave.

Signs of the battle between Maui and Kona were found higher on the Willow River. As Maui pushed his spear through the rocks to move the moʻo, he left a crater near a waterfall called Pukamaui Falls. But the Mugu escaped to another hiding place along the river to find and defend Maui again and again.

Finally, Kona found deep waters and hid in a series of swimming pools a short distance above Waiānuenue. Maui searches up and down the river and finally discovers moʻo but cannot reach it with his spear. But he had an idea.

Maui asked the volcano gods for some hot stones. Pele agreed to his request, and Maui threw them in the ponds. The water started to boil, burning the mando and forcing a kona to the surface. Maui continued the battle, eventually killing Kona and letting his body continue downstream over Wainoyu to rest in the pool below.

These sites are now located within Wailuku River State Park in two sections: Waiānuenue (Rainbow Falls), where Hina lived in the cave behind the waterfalls, and Boiling Pots, a series of deep swimming pools where Kona tried to hide, a little further – a river.

Both sites show the results of the lava flow from Mauna Loa that entered the Wailuku River channel nearly 10,000 years ago. The lava didn’t seem to fill the canal completely, and the water continued to flow over the flow as it cooled. This lava flow can be seen as an edge in Waiānuenue (and also forms the roof of the Heena Cave below).

The same influx hosts several “pits” in the boiling pot section of the garden. Over the past several years, potholes have been prevented from seeing due to the growth of various plant species. In the first pictures of the boiled pots area, the vegetation on its banks is low shrubs and grass, but in modern times tall paisley trees on the northern bank and many other tree types on the south bank obscure river views. But in the first few months of this year, the southern bank was cleared near the park, and now, these pots can be seen again. At times when the river is high and fast, the turbulent water that is pushed through the pots “boils” as the water flows.

Despite the name, the water is usually not hot. The only time in the recent history of the river that the water was heated was in 1855 and 1856 when the lava flow from Mauna Loa progressed across the saddle between this volcano and Mauna Kea. Lava flowed into the Wailuku River canal but did not cross it, four miles above Boiling Pots.

Even cold water can be dangerous and swimmers have drowned in the Willow River. The river channel is relatively narrow and deep so that the rain from the slope can cause the river to rise quickly and become very turbulent. This can happen even when the weather is sunny in the boiling vessels but the cloudy dark slope. Locals quickly learn that “if the mountain is black, go back.”

Volcano activity updates

Kīlauea volcano does not explode. The USGS Volcano alert level remains at NORMAL. Kīlauea updates are released monthly.

Kīlauea monitoring data for the past month show variable but typical rates of earthquake and ground deformation, low rates of sulfur dioxide emissions, and only slight geological changes since the end of volcanic activity in September 2018. The water lake at the bottom of Halema’uma ‘continues to expand and deepen slowly. For the latest information on the lake, go to the Internet.

Mauna Loa does not erupt and remains at the volcano alert level. This level of alert does not mean that an imminent eruption or that progression to an eruption from the current level of disturbances is certain. Mauna Loa updates are released weekly.

Last week, about 56 minor earthquakes were recorded under upper altitudes in Mona Loa. Most of these depths occurred at shallow depths of less than five miles. GPS measurements show slowly increasing peak inflation in the long run, in line with the magma’s supply of shallow volcano storage system. Gas concentrations and fumarol temperatures as measured in both cone sulfur and peak remain stable. Webcams show no changes to the scene. For more information about the current observation of Mauna Loa volcano, go to the Internet.

There were four events with three or more physical reports in the Hawaiian Islands during the past week: a 3.5-magnitude earthquake four miles east of Pahala at a depth of 19 miles on July 7 at 11:45 am HST, a 3.0-magnitude earthquake six miles east of Pahala At a depth of 19 miles on July 4 at 8:24 pm HST, an earthquake measuring 4.3 miles eight miles southwest of Verne Forrest at a depth of four miles on July 3 at 2:18 pm HST, an earthquake measuring 4.6 miles 9 miles from Fern forest at a depth of four miles on July 2 at 11:20 pm ET.

HVO continues to closely monitor Kīlauea and Mauna Loa for signs of increased activity. Send questions to [email protected].

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