The smoking Pali (cliffs) from last Monday’s lava tour.
The Jaggar Museum - perched on the edge of Kilauea Volcano’s Halemaumau Crater.
Lava at ocean entry near Royal Gardens
East Rift Zone, Puna, HI
Kilauea in the light of the full moon.
GPOYW - Magmatic edition
-Red hot earth juice
-Orange death taffy
-Raw island
-Exposed plate lubricant
-Hot mountain pimple pus
-Planety crust blood
-King Koopa’s moat filler
-Land batter
-Basalty lemonade
-Pele’s ejaculate
or
“Oh look, honey. The new acreage has heated floors!”
Yesterday we felt a 4.7 magnitude earthquake in the jungle that, according to the USGS website, originated about 6 miles directly south of the treehouse near Kilauea Volcano’s Pu’u O’o vent.
In Hawaii we have two kinds of earthquakes: Volcanic, which are caused by magmatic movements inside the volcanoes, and Techtonic, which originate from areas of structural weakness at the base of the volcanoes or deep within the earth’s crust.
Volcanic earthquakes are the most common and a relatively large one like we felt yesterday is often an indicator of upcoming volcanic activity. Nothing new on the USGS webcams yet, but I’m keeping my eyes peeled. Last spring Pu’u O’o went off like crazy and every night from the treehouse roof a bright red glow could be seen on the horizon.
Your mother’s back probably won’t break, but your foot will melt.
New lava near the ocean entry in the volcano park, day and nght.
Hanging out eating dinner around this is like being around the campfire but way more bad ass.
One can toss in a penny and watch it burst into flames when it hits the heat.
Kilauea from 6000 feet up Mauna Loa strip road.
