Eric Ignacio's photostream

EVERY SUNSET

Author: Jessica Voyles

Meeting you
was pure destiny,
You and I
were ment to be.

Maybe not now
but someday soon,
We'll meet not under the sun
but beneath the moon.

We'll watch the stars
'till they fade away,
but we won't fade
together we'll always stay.

This is the day
I'm waiting for,
from that day
I'll love you more and more.

I can't wait to watch
the sun set with you,
every sunset from that day
'till the rest of our lives are through.

Diamond Head is part of the complex of cones, vents, and their associated eruption flows that are collectively known to geologists as the Honolulu Volcanic Series, eruptions from the Koʻolau Volcano that took place long after the volcano formed and had gone dormant. The Honolulu Volcanic Series is a series of volcanic eruption events that created many of Oʻahu's well-known landmarks, including Punchbowl Crater, Hanauma Bay, Koko Head, and Manana Island in addition to Diamond Head.

Diamond Head, like the rest of the Honolulu Volcanics, is much younger than the main mass of the Koʻolau Mountain Range. While the Koʻolau Range is about 2.6 million years old, Diamond Head is estimated to be about 200,000 years old and extinct for 150,000 years.

The eruption that built up Diamond Head was probably very brief, lasting no more than a few days. It was probably explosive, since when the cinder cone was originally formed, the sea level is thought to have been higher and the vent burst erupted over a coral reef. Another factor probably contributing to the eruption's explosive nature was that rising magma would have come into contact with the water table. The eruption's relatively brief length is thought to explain why the cone today is so symmetrical.

A nearby eruption that took place at about the same time as the Diamond Head eruption was the eruption that built the Black Point lava shield. Since the type of eruptions that built Diamond Head tend to be monogenetic, geologists don't believe Diamond Head will erupt again.

This is the veiw from my back porch lanai... I love the sunsets.

In winter, Waimea and other North Shore locations such as Pipeline and Sunset Beach host a number of surfing contests because of the large waves found here. These waves are created by winter storms in the North Pacific, and their arrival on O‘ahu's North Shore are typically forecast accurately several days in advance. In summer, Waimea typically has clear and calm water.

The surf break at Waimea Bay was significant in the development of Big wave surfing. Larger surf at the bay went unridden for years until November 7, 1957 when a handful of surfers finally paddled out and rode the giant waves that break off the northern point of the bay. While the surf only breaks big several times a year, Waimea was the most prestigious big wave surf break in the world for decades. With the advent of tow-in surfing, more and more big wave breaks have been discovered that are far superior in quality than Waimea. However, the bay still holds a significant place even in today's world of big wave surfing.

Sunset over Waimea Bay, Hawaii on the North Shore of OahuThe Quiksilver Big Wave Invitational in Memory of Eddie Aikau takes place in this point to honour the legendary surfer and the first lifeguard of the North Shore of Oahu. Since its inception in 1984, the tournament has only been held seven times, due to a precondition that there be waves at least 20 feet high at Waimea Bay. The most recent tournament was in December 2004, when waves in the bay reached 30 to 50 feet high.

On January 28 1998, Hawaii issued its first ever "condition black" legally closing all North Shore beaches including Waimea bay. The Quiksilver Big Wave Invitational in Memory of Eddie Aikau was canceled do to above average behemoth surf.

Explore May 22, 2009 #224... Thank you everybody!