The lava has been flowing into the ocean for a little over a month now and all my photographer friends are posting great photos. It is really past time I got myself down to Kalapana to see the lava. The real problem is that my vehicle has been in the shop and I had no way to carry the bike. The answer? Don wanted to make another go at it, his bike rack holds two! Can you pick me up on your way past Waikoloa?
The 61G lava flow ocean entry at Kamokuna under the light of a full MoonWhile the lava is further from the end of the road than on my previous hikes, a full 4.5miles, it is actually easier to get to. When earlier flows looked like they would cut the main highway into Puna the county re-cut Chain of Craters road across the lava flows. The road is closed to motor vehicle traffic, but foot and bicycle traffic is allowed. This gives a direct access to the current 61G lava flow without having to cross country for miles across older flows.
Note! The contents of this posting are obsolete, there is currently no surface lava accessible on the island. When it does reach the surface again I will most likely be there, look to see an update of this article in the future!
The 61G flow reached the ocean a month ago, but only this last weekend did I get a chance to go out and see it for myself. It is quite a bit further to go than previous visits, about four and a half miles, but is it also much easier. I realized that my Getting to the Lava post is a bit outdated and a serious update is in order.
The 61G lava flow ocean entry at KamokunaThe 61G flow began on May 24th, breaking out on the southeastern flank of Pu’u O’o. The flow moved fairly quickly, cutting the re-built Chain of Craters Road and entering the ocean on July 26th. The flow is quite vigorous with an ample supply of lava. There are currently multiple surface breakouts and multiple ocean entry points. The flow is building new land near Kamokuna, the lava delta has added around 11 acres to the Big Island in one month.
Map of the 61G lava flow as of July 2ndWith easier access and a dramatic ocean entry the 61G flow is drawing large crowds of visitors that have come to see the spectacle. In my opinion the trip is very much worth the effort. Still, there are inherent risks in experiencing raw nature like this. A little preparation is in order and may prevent a visit from becoming an emergency.
One of the most striking features of Mauna Kea is the māmane forest. These native trees are generally found from 5,000-9,000ft elevation on the slopes of the mountain. The māmane (Sophora chrysophylla) is highly variable in appearance, growing as a shrub or a tree, bearing bright yellow flowers in late winter months.
At around 8,000ft there is a fence built to keep feral sheep and cattle out of the māmane forest and to protect the endangered palila (Loxioides bailleui). Above this fence the trees thrive, below the fence the forest is nearly dead. The hillsides scattered with relic trees where no young trees survive the herbivores to replace them. While desolate in appearance these old trees can be quite photogenic.
A skeletal māmane tree (Sophora chrysophylla) in the saddle region of Mauna Kea
A mamane tree along the Mauna Kea access road.
A dead grove of mamane on the side of Mauna Kea
The remains of an ancient mamane with a snow covered Mauna Loa behind
A mamane tree in the fog along Mauna Kea access road
A favorite mamane tree framed by a fogbow along the Mauna Kea access road
A mamane tree in heavy fog along the Mauna Kea summit access road
A thin crescent moon rises over the slopes of Mauna Kea at dawn