Hawaii 1999 Album - The Big Island |
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Trip #3, island #1For Sonia and I this was our third trip to the island of Hawaii, for Catherine, this was her second. We landed in Hilo, spent some time looking at the Liliuokalani Gardens, had dinner, and then drove up to the area near Volcanoes National Park where we stayed at the HaleKilauea B&B. Arriving in Hilo in the afternoon, I thought we would avoid the typical morning shower we had encountered previously. We did, only to find the occasional afternoon shower. Of course with daily rain the waterfalls are always running.
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| Hilo forecast: showers likely! "...as in daily." |
![]() Rainbow Falls | |||
The coast around Hilo is very beautiful. The daily showers (usually in the morning) give rise to lush vegetation and scenic beauty. The daily rain on the eastern side of the island also gives rise (or should that be 'falls') to many waterfalls. This one is Rainbow Falls. To me, the most dramatic falls are those that go right into the ocean. | ||||
| What happens when you hike in a rain forest! "...you get wet!" | Could this be the car from yesterday's hikers? | |||
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Okay, so it wasn't such a hot idea. The guide book said the KahauaLe'a Trail at the end of South Glenwood road to Pu'u O'o (lava source of the current flows) was an all day hike... but it was only 5 or 6 miles! How slow did these people walk anyway? Well we soon found out. The 'trail' (if you want to call it that) was well marked with colorful plastic strips, but there was a constant assortment of rocks, roots, ruts, twists, turns, ups, downs, and of course the mud! Oops! how could I have forgotten to mention the R A I N ! Our tennis shoes, even with careful steps were no match for the terrain. The got muddy and we got soaked. So after about 30 minutes, even I was ready to give up. Maybe another day when I have the right equipment. | |||
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The volcano vs. civilization "...volcano=1, civilization=0" When lava flows there is very little that stands in its way. The picture on the left above shows a 20 foot high flow of lava that went right over the road. The picture on the right is standing on top of the flow looking back to the road. The flow itself covered about a quarter mile of the road. This area is near the Kalapana area t the 'end' of Route #130 | ![]() | ||
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![]() | The colors evident in the cross section of the lava to the left are caused by minerals in the molten lava. The texture of the lava depends on the temperature to which it was heated, and the manner in which it cooled. Surface lava rock is generally very light and porous.
Of course it doesn't take nature long to begin making the barren lava into useful soil. Ferns are among the first colonizers of lava flows. Lava exposed to the air begins to cool. A variety of surface patterns form and are often later distorted by the continued movement of lava beneath the thin crust. Most major flow develop 'lava tube' which carry molten lava many miles from its source, usually down to the ocean. | |||
| The volcano vs. the ocean "...volcano=1, ocean=1" The contest is sort of a draw. There is no clear winner or loser. As you might expect, hot lava entering the ocean produces a lot of steam, but depending on the consistency and temperature of the lava, it may also cause the lava to explode into a fine gravel.... the birth of a 'black sand' beach. Back from the ocean the ferns do their thing. These pictures were taken near Kaimu. | ![]() |
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![]() ![]() | ![]() ![]() | Being in the middle of this island building process, a process which spans thousands of years, gives me pause... What is my life and what is it's impact on this earth? | ||
| The Western side of the island "compared to the East, it's a desert!" | ||||
Hapuna beach We came here twice, first the day we discovered it, then the second time we came back for the great snorkeling. |
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Detail Island links: |
Here are links to the detail photo pages in this series:
Need a guide book? We can recommend: Hawaii the big Island Revealed | |||
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