Honolulu, Hawaii - Video Travel on www.CheckMyCity.com

Honolulu, Hawaii

Honolulu is the capital and most populous census-designated place (CDP) in the U.S. state of Hawaii. Although Honolulu refers to the urban area on the southeastern shore of the island of Oahu, the city and the county are consolidated, known as the City and County of Honolulu, and the city and county is designated as the entire island. The City and County of Honolulu is the only incorporated city in Hawaii, as all other local government entities are administered at the county level. The population of the census designated place was 371,657 at the 2000 census, while the population of the City and County was 909,863. In the Hawaiian language, Honolulu means "sheltered bay" or "place of shelter."




History

It is not known when Honolulu was first settled by the original Polynesian migrants to the archipelago. Oral histories and artifacts indicate that there was a settlement where Honolulu now stands in the 12th century. However, after Kamehameha I conquered Oʻahu in the Battle of Nuʻuanu at Nuʻuanu Pali, he moved his royal court from the Island of Hawaiʻi to Waikīkī in 1804. His court later relocated, in 1809, to what is now downtown Honolulu.

Captain William Brown of England was the first foreigner to sail, in 1794, into what is now Honolulu Harbor. More foreign ships would follow, making the port of Honolulu a focal point for merchant ships traveling between North America and Asia.
In 1845, Kamehameha III moved the permanent capital of the Hawaiian Kingdom from Lahaina on Maui to Honolulu. He and the kings that followed him transformed Honolulu into a modern capital, erecting buildings such as St. Andrew's Cathedral, ʻIolani Palace, and Aliʻiōlani Hale. At the same time, Honolulu became the center of commerce in the Islands, with descendants of American missionaries establishing major businesses in downtown Honolulu.
Despite the turbulent history of the late 19th century and early 20th century, which saw the overthrow of the Hawaiian monarchy, Hawaiʻi's subsequent annexation by the United States, and the Japanese attack on Pearl Harbor, Honolulu would remain the capital, largest city, and main airport and seaport of the Hawaiian Islands.
An economic and tourism boom following statehood brought rapid economic growth to Honolulu and Hawaiʻi. Modern air travel would bring thousands, eventually millions (per annum) of visitors to the Islands. Today, Honolulu is a modern city with numerous high-rise buildings, and Waikīkī is the center of the tourism industry in Hawaiʻi, with thousands of hotel rooms.

Government

Completed in 1928, Honolulu Hale is the seat of the city and county.
Honolulu is administered under a consolidated city-county form of government employing a strong mayor-council system. The Mayor of Honolulu holds executive privileges — as opposed to mayors with only ceremonial powers — and the Honolulu City Council serves as the legislature. Mufi Hannemann currently serves as Mayor of Honolulu. His term ends January 2, 2010.
The city and county works with an annual operating budget of over USD 1.6 billion (2008 fiscal year.)[6] The Honolulu Fire Department and Honolulu Police Department are administered by the mayor and city council through appointed officials.
Source: Wikipedia

Diamond Head, Hawaii - Video Travel on www.CheckMyCity.com

Diamond Head, Hawaii

Diamond Head is the name of a volcanic tuff cone on the Hawaiian island of Oʻahu and known to Hawaiians as Lēʻahi, most likely from lae 'browridge, promontory' plus ʻahi 'tuna' because the shape of the ridgeline resembles the shape of a tuna's dorsal fin. Its English name was given by British sailors in the 19th century, who mistook calcite crystals embedded in the rock for diamonds.




Geology

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 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.
Source: Wikipedia