Mauna Loa, here I come!
My first trip to Mauna Loa started off at 6 am when Tyler, Jamal, Kelly and I left the lava house/dorm and headed down highway 11 to pick up Frank. We made it to Hilo a hour later and picked up coffee and bento's (to be explained later) from a Hawaiian fast food type joint. The only road to access Mauna Loa requires we drive from 4000' to sea level and then back up to 7000' in the saddle between Mauna Loa and Mauna Kea. Mauna Kea is the volcano almost directly north of Mauna Loa and is actually 100' taller above sea level. Mauna Loa is still the largest volcano in the world, however, because its roots and magma chamber are so massive that it causes the ocean crust to sag down about 5 km, adding overall height to the volcano.
We finally made it to the top and it was gorgeous! Mauna Kea (in the background) has not erupted for 4000 years and is in the shield forming volcano stage, producing alkalic lava (less partial melt of the crust as the magma rises to the surface). Frank was able to point out all the lava flows on the flanks of both Mauna Kea and Mauna Loa by date and eruption styles. In the saddle between the two volcanoes is a military training facility and bombing space.
Once parked, we made the short but stressful (because of the elevation change) hike over to the rim of the caldera. My initial reaction upon finally seeing it is inappropriate for younger audiences. One of the two projects I will be working on is taking about a hundred GPS measurements from within the crater, which is covered with lava from the 1984 eruption. The caldera is about 2 km by 6 km and not as flat as it looks. There is a cabin on the opposite rim of the crater for camping out to maximize the data collected in one trip.
Look! Snow in Hawaii! The greenish rock in front of the snow is pooled lava that was ejected from the crater during an explosive eruption. There are 5 types of explosive rocks and we spent about a hour learning them and their characteristics.
Check us out in our badass geology gear. Not sure why we are all standing around. The guy with his back to us is Frank - he avoided my camera all day.
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