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September 26, 2019 by Peter T Young 6 Comments

Mōʻiliʻili Karst

Prior and into the 1800s, Mōʻiliʻili was an agricultural community. It was transformed in the early 20th century into a self-contained town center with expanded businesses along King Street by Japanese immigrants who made Mōʻiliʻili their home.

This area is part of the Waikīkī ahupuaʻa.  Waikīkī was once a vast marshland whose boundaries encompassed more than 2,000-acres.  Here, the Mānoa and Pālolo streams (and springs in Mānoa (Punahou and Kānewai)) watered the marshland below.

With the arrival and settlement of the Hawaiians, this area gradually transformed from marsh into hundreds of taro fields, fish ponds and gardens.  The broad expanse of the Waikīkī ahupuaʻa was once one of the most productive agricultural areas in old Hawai‘i.

In the 1860s and 1870s, former Asian sugar plantation workers (Japanese and Chinese) replaced the taro and farmed more than 500-acres of wetlands in rice fields, also raising fish and ducks in the ponds.  By 1892, Waikīkī had 542 acres planted in rice, representing almost 12% of the total 4,659-acres planted in rice on O‘ahu.

During the 1920s, the Waikīkī landscape would be transformed when the construction of the Ala Wai Drainage Canal, begun in 1921 and completed in 1928, resulted in the draining and filling in of the remaining ponds and irrigated fields of Waikīkī.

Many residents of the Mōʻiliʻili area (and beyond) may not be aware that just a few feet below their feet, cars, houses and businesses are remnant caverns and caves (and water) in the Mōʻiliʻili underground.

During the island’s formative stage, the sea level was more than 25 feet higher than its present level. This period of sea level elevation is responsible for the deposit of fossil reef limestone in southern coastal Oʻahu, including up to the region we now know as Mōʻiliʻili.

The weathering and erosion of Oahu’s dormant volcanoes, the Waianae and Koʻolau, paired with the rise and retrieval of the sea level resulted in the formation of “interbedded marine and terrestrial deposits”.

The underground cave system is thought to be part of the original channel of Mānoa stream – people call it the Mōʻiliʻili Karst (Karst being a geological formation shaped by the dissolution of a layer or layers of soluble bedrock, such as limestone.)

The wide upslope section of the cave is centered near the intersection of University Avenue and South King Street (down slope from the University Avenue – H-1 interchange.)  The lower edge is located at the intersection of University Avenue and Kapiʻolani Boulevard.

The environment above the karst is highly urbanized, containing busy streets, buildings and businesses. The consequences of such urbanization are evident. Before damages due to urbanization and cave-ins, the Mōʻiliʻili Karst contained a half-mile cave that seemed to be a single connected structure.

There were several ponds that were fed by the karsic springs. One was located west of University Avenue, upslope of Beretania Street (near the UH makai campus.) The Kānewai underground pond was important to Hawaiian culture, because its water was said to have healing properties.

According to Hawaiian folklore, fish swam underground from the sea to this pool to eavesdrop on the fishermen who frequented this area and listen to the fishers’ plans.

Another important spring-fed pond was the Hausten (formerly Kumulae) pond. Originally, the pond was a favorite of Queen Kamāmalu (sister of Kamehameha IV and V).  The Queen and her brothers loved swimming in the ponds, which were also said to have healing powers.  The pond became the site of the Willows restaurant, and served as an attraction to customers there.

In 1934, a construction project downslope struck a master conduit of the karst. This caused massive water drainage of the upslope area; “for more than four months, an average of 3.8 x 107 L was pumped daily before the hole could be sealed and construction resumed.” The total amount pumped before the leak could be sealed was greater than one billion gallons of water.

The spring-feed ponds vanished within 24 hours.  There have been several instances of collapses since the dewatering. One instance in 1952 involves the Standard Trading store falling through the ground into the karst below it.  Another instance involves the emergence of a large cavern downslope from the King-University intersection.

The leak was repaired, but had changed the karst forever. Several spots in the formation were deliberately filled.  Cave-ins greatly reduced the size of the cave network, and changed access to the underground.

The Mōʻiliʻili Karst (Mōʻiliʻili Water Cave) is the only place where bare limestone can be seen; the cave is approximated to be as high as ten feet, and have depth of up to five feet in places.

It is entered by only by a drainage grate, and despite the impacts of human intrusion, “construction fill, metal pilings, and trash swept into the system by floodwaters,” the cave has been able to retain its cool and clear water.

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Filed Under: General, Place Names Tagged With: Hawaii, Karst, Moiliili, Waikiki

August 31, 2019 by Peter T Young 1 Comment

Māʻilikūkahi

Traditions on the island of O‘ahu provide the names of a dynasty of ruling chiefs beginning with Māʻilikūkahi, honored as the first great king of O‘ahu.

Māʻilikūkahi holds a prominent place in O‘ahu legends for his wise, firm, judicious government.

He was born ali‘i kapu at the birthing stones of Kūkaniloko; Kūkaniloko was one of two places in Hawai‘i specifically designated for the birth of high ranking children; the other site was Holoholokū at Wailua on Kauai.

Māʻilikūkahi, who ruled in the 1400-1500s (at about the same time Christopher Columbus ‘discovered’ America,) was raised partly in Waialua and is said to have maintained a kulanakauhale (village) there.

There is said to have been a mythical heiau (temple) called Kapukapuākea built by the menehune. Māʻilikūkahi was taken to Kapukapuākea (heiau) at Pa‘la‘akai in Waialua to be consecrated and installed as aliʻi there.

Kapukapuākea was to the Oʻahu aliʻi what Westminster Abbey is to the kings of England, the site of ritual acknowledgement of their divine right to rule (Kirch)

Soon after becoming aliʻi, Māʻilikūkahi moved to Waikīkī. The stories tell us that he was probably one of the first chiefs to live there. Up until this time the chiefs had typically lived at Waialua and ‘Ewa.

From that point on, with few exceptions, Waikīkī remained the seat of Oʻahu aliʻi, until Kamehameha I moved the seat to Honolulu.

Māʻilikūkahi was a religious chief, built several heiau, held the priests in honor and stopped human sacrifices. The island of Oʻahu is said to have become very populous during his reign, and thrift and prosperity abounded.

Land was considered the property of the aliʻi which he held in trust for the gods. The title of aliʻi ensured rights and responsibilities pertaining to the land, but did not confer absolute ownership.

The aliʻi kept the parcels he wanted, his higher chiefs received large parcels from him and, in turn, distributed smaller parcels to lesser chiefs. The makaʻāinana (commoners) worked the individual plots of land (kuleana.)

Māʻilikūkahi is noted for clearly marking and reorganizing land division palena (boundaries) on O‘ahu. Defined palena brought greater productivity to the lands; lessened conflict and was a means of settling disputes of future aliʻi who would be in control of the bounded lands; protected the commoners from the chiefs; and brought (for the most part) peace and prosperity.

Fornander writes, “He caused the island to be thoroughly surveyed, and boundaries between differing divisions and lands be definitely and permanently marked out, thus obviating future disputes between neighboring chiefs and landholders.”

Kamakau tells a similar story, “When the kingdom passed to Māʻilikūkahi, the land divisions were in a state of confusion; the ahupuaʻa, the ku, the ʻili ʻaina, the moʻo ʻaina, the pauku ʻaina, and the kihapai were not clearly defined.”

“Therefore, Māʻilikūkahi ordered the chiefs, aliʻi, the lesser chiefs, kaukau aliʻi, the warrior chiefs, puʻali aliʻi, and the overseers (luna) to divide all of Oʻahu into moku, ahupuaʻa, ʻili kupono, ʻili ʻaina, and moʻo ʻaina.”

What is commonly referred to as the “ahupuaʻa system” is a result of the firm establishment of palena (boundaries.) This system of land divisions and boundaries enabled a konohiki (land/resource manager) to know the limits and productivity of the resources that they managed – and increase its productivity.

Māʻilikūkahi is also known for a benevolent reign that was followed by generations of peace. He prohibited the chiefs from plundering the maka‘āinana, with punishment of death. His reign “ushered in an era of benign rule lasting for several generations.”

Māʻilikūkahi’s peaceful reign was interrupted by an invasion by chiefs from Waipi‘o. It was not considered as a war between the two islands, but rather as a raid by some restless and turbulent chiefs from the Islands of Hawaiʻi.

The invading force landed at first at Waikīkī, but, for reasons not stated in the legend, altered their mind and proceeded up the Ewa lagoon and marched inland.

At Waikakalaua (Wahiawa or Waipahu) they met Māʻilikūkahi with his forces, and a battle ensued. The fight continued from there to the Kīpapa gulch. The invaders were thoroughly defeated, and the gulch is said to have been literally paved with the corpses of the slain, and received its name, “Kīpapa,” (placed prone.)

Māʻilikūkahi’s wife was Kanepukaa. They had two sons, Kalonanui and Kalona-iki, the latter succeeding his father as Aliʻi Aimoku of Oʻahu.

In the past, MAʻO Organic Farms created and facilitated ‘Āina Ho‘ōla o Māʻilikūkahi, the annual statewide Hands Turned to the Soil conference. The word ho‘ōla means to restore/give life.

The conference’s name therefore reflects an understanding that our ‘āina must itself be healthy in order to feed us and that ‘aina, kanaka and kaiaulu (land, people and community) work in concert to provide and maintain sustenance for all living things.

In 2018, the University of Hawai‘i – West Oahu Sustainable Community Food Systems Program, the Sustainable Agriculture Education Association, the University of Hawai‘i System Office of Sustainability and key community partners hosted the 2018 Sustainable Agriculture Education Association Conference and the Hoʻōla ʻĀina O Māʻilikūkahi Youth Food Sovereignty Congress.

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Filed Under: Ali'i / Chiefs / Governance, Place Names Tagged With: Ewa, Hawaii, Kukaniloko, Mailikukahi, Oahu, Waikiki

August 17, 2019 by Peter T Young 1 Comment

Sands of Time

Waikīkī is a ‘built’ beach.

Over the last 100-years it has been built primarily in two ways, (1) construction of walls and groins in the nearshore waters and (2) beach nourishment/replenishment (adding sand to the beach.)

Between 1913-1919, the majority of Waikīkī had seawalls; they were placed to protect roadways and new buildings. The beach was lost fronting Kūhiō and Queen’s Beach.

In 1927, the Territorial Legislature authorized Act 273 allowing the Board of Harbor Commissioners to rebuild the eroded beach at Waikīkī. By 1930, the Board of Harbor Commissioners reported on construction progress, which included 11 groins along a portion of the shoreline.

Then, they started adding sand to Waikīkī Beach.

Reports from the 1920s and 1930s reveal that sand was brought in to Waikīkī Beach, via ship and barge, from Manhattan Beach, California.

As the Manhattan Beach community was developing, it found that excess sand in the beach dunes and it was getting in the way of development there. At the same time, folks in Hawai‘i were in need for sand to cover the rock and coral beach at Waikīkī.

Kuhn Bros. Construction Co supplied the sand; they would haul the sand up from Manhattan Beach, load it onto railroad cars, have it transported to the harbor in San Pedro and shipped by barge or ship to Hawai‘i.

Later, Waikīkī’s sand was trucked from various points around Hawai‘i including O‘ahu’s North Shore – in particular, Waimea Bay Beach, a sand bar off the town of Kahuku and Pāpōhaku Beach on Molokai.

Reportedly, before sand mining operations removed over 200,000 tons of sand at Waimea Bay to fill beaches in Waikīkī and elsewhere, there was so much sand that if you would have tried to jump off Pōhaku Lele, Jump Rock, you would have jumped about six feet down into the sand below.

A formal application for a cooperative study regarding beach erosion in Waikīkī was made by the Board of Harbor Commissioners, Territory of Hawaii in 1948.

The intent of the Waikīkī Beach Erosion Control Project, which was the responsibility of the Army Corps of Engineers, was to increase beach land, improve access to beaches, and to prevent further erosion of beach sand.

The Waikīkī Beach Erosion Control Project was initiated in response. This project initiated what would turn out to be a 50-year series of attempts to restore Waikīkī Beach.

Since 1929, about 616,500 cubic yards of sand have been used to enlarge and replenish Waikīkī Beach between Fort DeRussy and Kūhiō Beach, but every year more erodes away. Little sand has been added since the 1970s, according to the DLNR.

When I was at DLNR, we initiated a demonstration project to move near shore sand back on to the beach.

In 2006, DLNR spent $500,000 to siphon 10,000 cubic yards of offshore sand – this was the largest replenishment effort of Waikīkī’s beaches in more than 30 years.

It worked; then, a larger project was implemented.

Early in 2012, a larger-scale replenishment project pumped sand from 2,000 feet off Waikīkī to fill in the shrinking beach.

The 2006 demonstration project and recent (2012) larger scale replenishment were really recycling projects, because the sand now settled offshore was brought in years ago to fill out the beach.

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  • Waikiki-fronting_old-Seaside_Hotel-seawall-1915
  • Waikiki with Diamond Head in the background-hawaii-gov-1934
  • Waikiki_and_Helumoa_Coconut-(from_Ewa_end_of_Helumoa)-1870
  • Waikiki_Beach_Houses_(UH_Manoa)-1924
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Filed Under: General Tagged With: Beach, Hawaii, Sand Replenishment, Waikiki

July 19, 2019 by Peter T Young Leave a Comment

Rice

Rice production was not a major contributor to Hawaiʻi’s economy until the latter half of the nineteenth century. As whaling declined in importance, greater emphasis was placed on agricultural production, primarily sugar and rice.

It was in 1850 when the Royal Hawaiian Agricultural Society was formed to develop Hawaiʻi’s agricultural resources that rice made its mark in the Hawaiʻi economy. The group purchased land in the Nuʻuanu Valley and rice seed from China and planted in a former taro patch.

At first the Society offered the rice seed to anyone in Hawaiʻi who wanted to plant it. King Kamehameha IV also offered land grants for cultivation of rice. Because there were no proper milling facilities in Hawaiʻi, it didn’t take off as a viable crop right away.

Then, in 1860, imported rice seed from South Carolina proved very successful and yielded a fair amount of crop. This, combined with the collapse of the taro industry in 1861-1862 (as the Hawaiian population declined, the demand for taro also declined,) added value to the numerous vacant taro patches and a boom in the rice industry.

From 1860 to the 1920s, Rice was raised in the islands of Hawaiʻi, particularly in Kauai and Oʻahu, because of their abundance of rain.

The Hanalei Valley of Kauai led all other single geographic units in the amount of acreage planted in rice. The valley was one of the first areas converted to this use and continued to produce well into the 1960s.

The Commercial Pacific Advertiser noted on October 3, 1861, “Everybody and his wife (including defunct government employees) are into rice – sugar is nowhere and cotton is no longer king. Taro patches are held at fabulous valuations, and among the thoughtful the query is being propounded, where is our taro to come from?”

During the 1860s and 1870s, the production of rice increased substantially. It was consumed domestically by the burgeoning numbers of Chinese brought to the Islands as agricultural laborers.

In 1862, the first rice mill in the Hawaiian Islands was constructed in Honolulu (prior to that it was sent unhulled and uncleaned to be milled in San Francisco.) By 1887 over 13 million pounds of rice were exported.

A particularly important stimulus for the increased demand for rice was the Reciprocity Treaty of 1876. This treaty between the United States and the Kingdom of Hawaiʻi granted duty-free status to certain items of trade between the two countries, including rice.

Thomas Thrum wrote in 1877 that Kamehameha V and other landowners had “planted a large tract of land in rice (in Moanalua,) and even went so far as to pull up and destroy large patches of growing taro to plant rice.”

In 1899, Hawaiʻi’s rice production had expanded so that it placed third in production of rice behind Louisiana and South Carolina.

Much of this rice acreage was worked initially by Chinese immigrants, who first arrived as contract laborers in 1852. By 1860 this immigrant population totaled 1,200. Chinese immigration continued at a rapid pace until 1884, when the official census estimated the number of Chinese at 18,254.

In 1882 the US Congress passed the Chinese Exclusion Act; then, Japanese workers were brought in to take their place. Within only five years the Japanese constituted more than forty-two percent of the plantation work force and one-seventh of the total population.

Ironically, this influx of Japanese immigrants accelerated Hawaiʻi’s decline in rice production. Japanese preferred short grain rice rather than the long grain rice the Chinese were used to eating. So rice began to be imported from California for the Japanese.

California’s success would ultimately mean the end of the rice industry in Hawaiʻi. Furthermore, the hand labor techniques of Hawaiʻi’s Chinese and Japanese rice farmers could not compete with California’s mechanized production technology.

Additional problems with the rice bird and rice borer, as well as the lack of interest on the part of the younger generation to continue rice farming, eventually meant the end of a once prosperous industry.

Attempts to revive rice production by the Agricultural Extension Service of the University of Hawaiʻi were made in 1906 and 1933, primarily in Hanalei.

As a result the acreage planted in rice on the island rose from 759 acres in 1933 to 1,058 in 1934. For areas like Hanalei Valley, such efforts, coupled with the valley’s general remoteness and absence of competing demands for the land, allowed rice cultivation to continue as a regional activity long after it had been abandoned throughout the rest of Hawaiʻi.

Today, there is no trace of the rice fields in Hawaiʻi. However, Hoʻopulapula Haraguchi Rice Mill museum in Hanalei Valley provides a remnant look at the once prospering agricultural venture.

It was built by the Chinese and purchased by the Haraguchi family in 1924. The Haraguchi family has restored the mill three times; after a fire in 1930, then again after Hurricane Iwa in 1982 and Hurricane Iniki in 1992.

The mill ceased operating in 1960 when Kauai’s rice industry collapsed. A nonprofit organization was formed to preserve and interpret the mill, which has been visited by thousands of school children and adults in the past 29 years.

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Rice
Rice
Rice
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View of rice fields towards Pālolo Valley from the back of Waikīkī, Hawai`i, ca. 1910
View of rice fields towards Pālolo Valley from the back of Waikīkī, Hawai`i, ca. 1910
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Windward_Rice_Planting
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Rice_fields_workers_beneath_Punchbowl_Crater,_Honolulu,_in_1900
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The Iron Horse Comes to Hawaii-Peter Hurd-1889
The Iron Horse Comes to Hawaii-Peter Hurd-1889
Chinese water buffalo plowing rice field Hawaii Tai Sing Loo-(KSBE)=
Chinese water buffalo plowing rice field Hawaii Tai Sing Loo-(KSBE)=
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Chinese-Waterbuffalo-Rice
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Filed Under: Economy Tagged With: Hanalei, Hawaii, Kaneohe, Rice, Waikiki

July 18, 2019 by Peter T Young 1 Comment

Lēʻahi

Lēʻahi, also known as Diamond Head, is a nearly circular crater of approximately two-thirds of a mile in diameter.

Diamond Head is different things to different people:
• Homes of Hawai‘i’s Kings, Queens and Royal Families were in its shadow
• It’s an internationally-recognized visitor industry icon
• It’s the backdrop to the famous Waikīkī Beach
• It served an integral role in the island military defenses
• It is present home and command center for State Civil Defense
• It’s an easy walk to the summit for spectacular views of the ocean and coastline
• It is a backdrop to a transformation of social, political and religious events

Diamond Head was given its name by British sailors who found natural calcite crystals on the slopes of the mountain and mistook them for diamonds. Hawaiians called the volcanic cone Lēʻahi, Laeʻahi or Lae-ahi. Translations include: “brow of the ʻahi” and “cape of fire.”

In the legend of Pele and Hi‘iaka, Hi‘iaka is said to have compared Diamond Head to the brow of the ‘ahi: Me he i‘a la ka Lae o Ahi; E kalali au ae nei i ke kai – Like a fish is the Brow-of-the-ahi Resting high above the sea.

Other names for Diamond Head include Point Rose (given to the geologic feature in 1786 by Captain Nathaniel Portlock in honor of the secretary of the British treasury), Diamond Hill and Conical Mountain.

Geologically speaking, Diamond Head is a dormant volcanic tuff cone, with a variable-height rim surrounding the recessed interior area; the eruption of Diamond Head took place well over 150,000-years ago.

The highest point (at 761-feet) on the southwest rim of Diamond Head is known as Lēʻahi Summit (most of the rim is between 400-500-feet.) The crater is on the southern coastline of Oʻahu, approximately one-and-a-half miles south of the Koʻolau range.

From at least the 15th century, chiefly residences lined the shore of Waikīkī, and cultivated fields spread across the Waikīkī plain to the foot of the crater and inland to the Ko‘olau valleys. There were several heiau in Waikīkī, of which several were located around Diamond Head.

One of Kamehameha’s main heiau (also suggested as a surfing heiau,) Papaʻenaʻena (also called Lēʻahi Heiau,) was situated at the base of the southern slopes.

Other heiau in the vicinity include Kupalaha Heiau, which may have been connected with Papaʻenaʻena, Pahu-a-Maui Heiau on the crater’s eastern cliffs overlooking the ocean (the site of the present Diamond Head lighthouse), Kapua Heiau near the present Kapiʻolani Park, and Ahi Heiau on the peak of Diamond Head.

In the early years of the 19th century, people tended gardens in the crater and one visitor described finding “an abundance of melons and watermelons growing wild, upon which we feasted”.

In 1831, the botanist, Dr. FJF Meyen, noted the crater contained a small pool of water “which was completely covered with plants”. (The crater pond was filled-in by military bulldozing; now, there is a seasonally-moist wetland where standing water can occasionally be seen.)

Some have suggested there is little likelihood for archaeological sites of pre-contact Hawaiian or early post-contact origin in the crater. The archival research suggests that the only Hawaiian activity that might have taken place in the crater was dryland farming (dating to 1822.)

In the Great Māhele division of lands between the king and his high chiefs, Diamond Head, which lies within the ¬ʻili of Kapahulu in the ahupua¬ʻa of Waikīkī, was awarded to William C. Lunalilo, the future king of Hawaiʻi (1873-1874).

In the early 1860s, Mark Twain commented, “On the seventh day out we saw a dim vast bulk standing up out of the wastes of the Pacific and knew that that spectral promontory was Diamond Head, a piece of this world which I had not seen before for twenty-nine years.”

“So we were nearing Honolulu, the capital city of the Sandwich Islands – those islands which to me were Paradise; a Paradise which I had been longing all those years to see again. Not any other thing in the world could have stirred me as the sight of that great rock did.”

In 1884, the Kapahulu portion of Lunalilo’s Māhele award was subdivided by the Lunalilo Estate. Diamond Head was transferred from the estate to the Hawaiian Government.

The summit of Lēʻahi affords an excellent and unobstructed view of the ocean from Koko Head in the east, to beyond the ʻEwa Plain to Wai‘anae in the west. The utility of Diamond Head did not go unnoticed by the U.S. Army.

In 1906, the US government acquired the 729-acres of Lunalilo’s property from the Hawaiian Government, as well as other adjacent lands (including Black Point), to create Fort Ruger Military Reservation, the easternmost of the coastal defense forts.

From 1963 to 2001, the FAA had its air traffic control facilities in Diamond Head crater, which guided Hawai‘i-bound aircraft from 250 miles outside the Islands to within 20 miles of their intended airport.

Diamond Head State Monument was first officially established under an Executive Order by Hawaiʻi’s Governor Quinn in 1962; nearly 500-acres of land now make up the Monument.

This early designation covered about 145-acres in a horseshoe configuration preserving the famous profile and the south and west exterior slopes from the crater rim down to Diamond Head Road. Subsequently, Executive Orders have added additional lands to the Monument.

The interior of the crater had been closed to the public from 1906 until 1968. (Remember the Sunshine Festivals back then?) In 1976, DLNR’s Division of State Parks became the agency responsible for the planning and management of the Monument – it is now open every day.

Two major tunnels (Kāhala Tunnel and Kapahulu Tunnel) provide pedestrian and vehicular access into the crater.

Two separate trail systems (interior and exterior) address different needs and purposes. The exterior trail system has a dual function as a jogging and bicycle path traversing the mauka end of the Monument and along the existing trail on the lower ʻEwa-makai slopes. The interior trail system leads to the summit of Lē¬ʻahi (1.6-mile round trip.)

Diamond Head is open daily 6 am to 6 pm, every day of the year including holidays, with entrance Fees of $5.00 per car or $1 per person for pedestrians (the money goes to State Parks.) Mountain Biking is not allowed on this trail. No dogs allowed in Diamond Head State Monument.

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Overlooking Waikiki-1929
Overlooking Waikiki-1929
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Waikiki-Diamond_Head-1940
1935 Chevrolet convertible with Diamond Head and Waikiki Beach in the background
1935 Chevrolet convertible with Diamond Head and Waikiki Beach in the background
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Waikiki_Beach-Boats-1935
Waikiki with Diamond Head in the background-hawaii-gov-1934
Waikiki with Diamond Head in the background-hawaii-gov-1934
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Joseph_Dwight_Strong_-_’View_of_Diamond_Head’,_oil_on_canvas-1880s
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Joseph_Dwight_Strong_-_’Hawaiians_at_Rest,_Waikiki’,_oil_on_canvas,_c._1884
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Diamond_Head-LOC-aep-his180
'Diamond_Head_from_Waikiki',_oil_on_canvas_painting_by_Enoch_Wood_Perry,_Jr.,_c._1865
‘Diamond_Head_from_Waikiki’,_oil_on_canvas_painting_by_Enoch_Wood_Perry,_Jr.,_c._1865
Diamond Head & Honolulu from the Punchbowl-(vic&becky)-1953
Diamond Head & Honolulu from the Punchbowl-(vic&becky)-1953
Automobile with Diamond Head and Waikiki in background, 1933
Automobile with Diamond Head and Waikiki in background, 1933
Alexander_Scott_-_Diamond_Head_from_Tantalus',_oil_on_canvas,_c.1906-8
Alexander_Scott_-_Diamond_Head_from_Tantalus’,_oil_on_canvas,_c.1906-8
Clipper plane passes Diamond Head-1935
Clipper plane passes Diamond Head-1935
Diamond_Head_Lighthouse-Transpac_Finish
Diamond_Head_Lighthouse-Transpac_Finish
Diamond Head

 

Filed Under: Place Names Tagged With: Crater Festival, Diamond Head, Fort Ruger, Hawaii, Leahi, Sunshine Festival, Waikiki

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Images of Old Hawaiʻi

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