Hawai'i, by far the largest of the Hawaiian Islands with
over 60% of the landmass, is also the youngest, which is why it has pretty much
all of the volcanic activity. Our tour guide, Harvey, explained that these
islands have been created not by the huge blast-style eruptions of volcanoes
like Mt. Etna, Mt. St. Helen's and the Icelandic volcanoes, but by a slow and
almost continuous seeping of magma from a hot spot below the Earth's crust. This
hot spot sits in the middle of the Pacific tectonic plate, rather than at the
edge of one, and the plate actually moves over it. The heated magma burns a
hole in the plate and then bubbles or spews out to form lava cones. These cones
eventually break the surface of the ocean and become volcanic islands. When the
magma flow ebbs, the hot spot cools off a bit and the island literally breaks
away from it, staying attached to the ocean floor, and is taken away as the
tectonic plate shifts. When the magma heats up enough, the cycle starts again
and another island is formed.
The Pacific plate is moving at about 6 inches per year in a
northwesterly direction, and this is why the Hawaiian islands are strung out
the way they are. Kauai is the oldest of the large islands at about 5 million
years, and The Big Island is the youngest at about 1 million years.
That being said, our first day here started with a trip to
Volcanoes National Park to see THE active volcano, Kilauea, up close. The active crater that opened up with a sudden eruption in 2008, is called Halemaumau. This is
the only continuously erupting volcano; you might recall that last fall there
was an eruption that destroyed a number of homes and threatened a small town,
but fortunately stopped only about a mile short. Harvey showed a National Parks
documentary on the last ten years' or so of Kilauea's history; it is amazing to
see close up how geologically active the Earth still is. It was even more
amazing to stand at the edge of Kilauea and watch her spew gases. If we had
been there in the evening, we would have seen the active crater glow red from
the extreme heat.
The gases rising from the active Halemaumau crater |
Anybody who's been around for a while knows where this came from! They were trying to figure out where to do this pose - on top of a volcano seemed a good spot! |
This area glows red at night. |
At the side of the road - steam vents from the active area. |
Our next stop was at the Thurston Lava Tube. These tubes are
created when a thick portion of the top crust of a lava flow cools faster than
what is underneath, and becomes a tunnel. The flow of lava peters out
eventually, and instead of blocking up the tunnel, it leaves a tube behind.
Did we mention that it was raining, again, when we got to
Hilo and the bus? Fortunately, the rain stopped while we were at the Kilauea
summit, but it started again just as we arrived at the lava tube. Now, this
wasn't the first rain they had had on Hawai'i this week; the weather here was
pretty much the same as everywhere else in the state. We all pulled on our rain
gear (in most cases a green plastic poncho from the local tour company), and
headed out. What nobody told us was just how porous lava is! We thought we
would at least be dry as we made our way through this 400 foot long
tunnel...but, no, it was probably wetter inside than it was outside! Barb has some
photos from inside, but, suffice it to say that some of the puddles were so big
that nobody got out the other end with dry feet!! We spent so much time
watching our steps that we couldn't really take in the sheer size of the tube.
The forest leading up to the lava tube |
The tube entrance. See how our rain ponchos match the colour of the foliage? |
Outside again. |
Of course, once we got back on the bus it stopped raining -
again. Our next stop was at the black sand beach at Punaluu, also famous for
the Green Sea Turtles that like to bask there in the sun. Because the beach is
made from lava that flowed all the way into the sea and was then crushed
against the shore, it has a different consistency. It is smooth instead of
sharp and if you pick some up in your hand it will all fall through your
fingers without sticking, unlike regular beach sand.
We did come across two sea turtles who barely blinked an eye
at the people wandering around them.
At the beach. One wouldn't think a warning would be necessary... |
The sea turtles |
The puahoehoe lava - smooth rather than sharp and rocky - that flowed in this area |
We finally reached the resort in the later afternoon, during
yet another downpour. This one came with lightning out over the ocean as well.
We felt lucky to have been able to get dinner at all, since the main restaurant
in the resort included outside tables, and the rain had rendered them unusable
for the evening. Not having a reservation was a difficulty, but we ultimately
were able to sit down for a meal.
The next morning, Harvey took us to the Kona Coffee Living
History Museum. It was here where we learned about the history of the
particular type of coffee grown on Hawai'i and particularly in the Kona area.
Kona Coffee farms were originally established by Japanese immigrants when they
arrived in Hawai'i in the 1800s. One couple who ran a farm for many, many years
donated their homestead to be used as a living museum when they retired. He has
since passed away, but his wife, who will be turning 101 soon, now lives on
Oahu. She had continued to run the homestead on the farm in the traditional way
until 1996.
The coffee plants. Red berries are ready to pick |
By the cleaning and drying shed |
The homestead |
Drying the washed beans on the shed roof before roasting. |
They grew lots of other things here, too. This is a baby pineapple plant. |
This gentleman was showing us how the beans were roasted. He owns a few acres and with some staff produces some Kona coffee. He is also about 91 years old - something none of us could ever believe. |
The kitchen in the homestead. Very traditional with no modern gadgets. The last owner of the house worked this kitchen in this way until only 20 years ago. |
We can't close the post without a few photos from around our
resort - the Sheraton at Keahou Bay. It was a very nice resort but not close to
very many things if you wanted to go off-site for shopping or a meal.
Kailua-Kona is the closest town, about 20 minutes by hotel shuttle. But it was
a lot quieter than Waikiki!
The resort from the road to Kona |
The hotel has a huge water slide. All of us (yes, all of us including Larry) had a go. Here's Barb just coming off the en |
Saturday afternoon and evening would be dedicated to Mauna
Kea - as will the next blog post!
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