Day 25 : Nahwiliwil - The Island Of Kauai
The Hawaiian islands sit in the middle of the Pacific tectonic plate. They lie over a hot spot (just like Yellowstone), where magma from deep down pushes to the surface. The hot spot remains in one place while the plate moves NorthEast at the rapid pace of 8cm (3 inches) per year. If you track all this on a map, you'll see that Kauai is the oldest of the islands, formed some 5 million years ago, while the Big Island of Hawaii is still being formed by the eruptions of Mauna Loa and Kilauea. There is also an undersea seafloor volcano, Lohi, some 20+ miles SE of the Big Island, that will eventually become the youngest island in the chain. This means that Kauai has had time to mature, with the resultant greenery - and is known as the Garden Isle. After five long days at sea, with up to 15-foot swells and 45-50mph gusts, it was an absolute pleasure to set foot on dry land. We approached the harbor in Nahwililwili Bay at about 8 am in the morning, with the sun almost due astern of us. We...