Images of Old Hawaiʻi

  • Home
  • About
  • Categories
    • Ali’i / Chiefs / Governance
    • American Protestant Mission
    • Buildings
    • Collections
    • Economy
    • Missionaries / Churches / Religious Buildings
    • General
    • Hawaiian Traditions
    • Other Summaries
    • Mayflower Summaries
    • Mayflower Full Summaries
    • Military
    • Place Names
    • Prominent People
    • Schools
    • Sailing, Shipping & Shipwrecks
    • Voyage of the Thaddeus
  • Collections
  • Contact
  • Follow

November 1, 2018 by Peter T Young Leave a Comment

The Islands in 1856

“On Owhyhee, two enormous mountains rise to 14,000 feet above the level of the sea, and rest crowned with perpetual snow. Many craters of extinct volcanoes, and extensive plains covered with the rude debris of earlier or later eruptions, exist everywhere; and Kilauea, on the mountain of Mouna Kea, is the largest active volcano in the known world.”

“In a country thus formed, and, doubtless, at a date comparatively so recent, we cannot be surprised that no metals have been found, and no minerals save the varieties of the lava, and some limestone which has been lately discovered lying in a remarkable and raised bed at Kahuku, in the island of Woahoo.”

“In this island there is also a salt-lake, a little elevated above the surface of the sea. Soils formed of such materials as those which thus compose the entire bed of the islands, could not be expected to be very fertile, save upon some of the lower or little elevated lands, and in the valleys long formed in situations exposed to the winter rains.”

“The climate generally of the islands is remarkable for its salubrity and its even temperature. Near the sea, the highest elevation of the thermometer is 86° Fahrenheit, and the lowest 62°. The greatest heat occurs during the month of July, and the least in January.”

“Thus the extreme range during the year, does not exceed 24°, but the variation is rarely more than 8°. The inhabitants may, however, by ascending to the higher lands, live in any temperature between that of these tropical latitudes and that of the frigid zone.”

“But, notwithstanding the general healthiness of the climate, at the time that the trade-winds are irregular, which happens during the winter months …”

“… when the wind is commonly from the south, rains and storms occur, attended by diseases not differing much from those which prevail in the southern parts of Europe, at the same season — such as headaches, rheumatism, and others, arising from imprudent exposure to the night air, in damp and chilly weather.”

“According to the reports of naturalists who have visited the islands, the spontaneous productions of their soil are much more varied than the evidently recent formation of the group would lead us to expect. It will suffice to mention, that those of the family of Rubiaceae, Con tor tee, and Urticae, predominate.”

“From the last of these, as well as from the Broussonetia papyrifera, or the paper mulberry, are made cordage and cloths. The acacia also abounds in the mountain districts, and is employed by the natives in the construction of their canoes.”

“The sandal-wood was also once very abundant, and lately afforded an article of commerce with the Chinese, by whom it is chiefly used for cabinet purposes. It is now, however, save some young, and, for the present, useless trees, quite destroyed.”

“The more familiar plants and useful productions for domestic purposes are, the banana-tree, the sugar-cane, the yam, the bread-fruit, and the taro-root (Arum esculentum), all of which are indigenous.”

“Such were these islands after they first raised their towering heads above the waters of the mighty ocean which surrounds them, and such the earliest productions of the vegetable world which sprung from the soil first formed.”

“Several important plants have been lately introduced, such as the coffee, cotton, rice, tobacco, the melon and water-melon, indigo, and even the vine, of which, however, though it flourishes in the mountain districts, little use is likely to be made, on account of the necessity of discouraging the growth of everything from which alcohol may be distilled.”

“Several of our ordinary vegetables have also been introduced with success, as well as some of the fruits of the tropical and temperate latitudes which were not indigenous, such as pine-apples, oranges, grapes, peaches, figs, tamarinds, and guavas. The bread-corns will also flourish on the higher lands.”

“With respect to the animal kingdom, it seems that at the discovery of the islands nothing was observed save hogs and dogs, the importation, without doubt, of the first inhabitants, and such of Nature’s earlier productions as may be considered habitants rather of the sea than of the land …”

“… but all our domestic animals, including such as we use for food, for beasts of burden, and for companions of our sports, have been since introduced.” (All here is from Hill.)

Follow Peter T Young on Facebook 

Follow Peter T Young on Google+ 

Follow Peter T Young on LinkedIn  

Follow Peter T Young on Blogger

© 2018 Hoʻokuleana LLC

Hawaiian Islands from Hill-1856
Hawaiian Islands from Hill-1856

Filed Under: Economy, General, Place Names Tagged With: Hawaii, Timeline, 1856

October 28, 2018 by Peter T Young 2 Comments

Koʻolau Volcano

O‘ahu used to be nearly twice as big as it is now. (Thompson) The Island consists of two major shield volcanoes: Waiʻanae and Koʻolau; the eroded remnants of which are the Waiʻanae Range and the Koʻolau Range.

Waiʻanae is the older of the two (breaking the ocean surface ~3.9 to ~2.8 million-years ago) and makes up the western part of O‘ahu. Koʻolau volcano started as a seamount above the Hawaiian hotspot around 4-million years ago. It broke sea level some time prior to 2.9-million years ago.

Koʻolaupoko, one of O‘ahu’s six ancient moku (districts,) is bounded by Kalaeoka‘ō‘io, which is a point near the center of the northeast coast at Kualoa; the crest of the Koʻolau Range to the west; and Makapuʻu Point on the southeastern tip of the island.

This expanse also generally delineates the extent of Koʻolau Volcano – effectively from and including Kāne‘ohe to Kailua to Waimānalo. A significant landslide and ongoing erosion reshaped the volcano.

About 2-million years ago, much of the northeast flank of Koʻolau volcano was sheared off and material was swept onto the ocean floor (named the Nuʻuanu Avalanche) – one of the largest landslides on Earth.

The Pali is the remaining edge of the giant basin, or caldera, formed by the volcano. At its base are the towns of Kāne’ohe, Kailua and Waimānalo – beyond that, open ocean. The other half of the caldera, an area the size of Brooklyn, tore away and tumbled into the ocean. (Sullivan)

Material swept more than 140-miles north of O‘ahu and Molokai. For the last 85-miles of its journey, the avalanche traveled uphill by about 1000 feet, leaving jumbled blocks – once part of O‘ahu – scattered over more than 9,000-square miles of seafloor. (Sinton)

Residual ridges, remnants of the old Koʻolau volcano, extend northeast from the Pali. These include the Mokulua islands, Olomana, Kapaʻa (where the quarry is,) Mahinui (Oneawa, Kalaheo) and Keolu Hills.

Mōkapu Peninsula (where Marine Corps Base Hawai‘i is situated) is evidence of subsequent secondary volcanic eruptions that formed Ulupaʻu Crater (the large hill on the Kailua side of the peninsula,) Pu‘u Hawaiiloa (the central hill that originally had the base control tower, now has radar (‘the hill’,)) Pyramid Rock and the nearby Moku Manu (Bird Island.)

Following a period of dormancy, Koʻolau erupted about 1-million years ago (known as the Honolulu Volcanic Series) and created landmarks such as Lēʻahi (Diamond Head,) Hanauma Bay, Pūowaina (Punchbowl Crater) and Āliapaʻakai (Salt Lake.) Another tuff cone is Mānana Island (Rabbit Island.)

Pounded by the tradewind and rains, the windward side of O‘ahu is more weathered than the leeward areas of the island, and now this vast caldera wall is reduced to a line of sheer cliffs stretching from Makapuʻu to Kualoa and beyond.

The flat valley floors are extensively eroded, and are now mostly joined, studded here and there with isolated remnant peaks and ridges connected to the central range. (Klieger)

Coral reefs and marine terraces were formed at different elevations due to the changing sea levels over time. There are some broad lowland areas in the lower reaches of deeply alluvial valleys. (Moberly)

It was the broadness of this coastal plain (which included swampy areas near the shore) that distinguished Koʻolaupoko from other areas of O‘ahu, and most likely helped account for the intensity and productiveness of agriculture.

The abundant rainfall produces constantly flowing streams that supported the vast expanse of wetland kalo (taro) lo‘i (pondfields) that once extended throughout Koʻolaupoko. (Klieger)

Because Kāne’ohe Bay has a deep lagoon between an outer reef and the shore, the reef is considered by some geologists to be a barrier reef, the only example in Hawaii. Several fishponds lined the bay.

Mokoliʻi (Chinaman’s Hat) and Mokuoloe (Coconut Island) are erosional remnants of the bedrock Koʻolau basalt; Kapapa and Kekepa (Turtleback) Islands are of limestone; and Ahu O Laka Island is a sand bar that is uncovered at low tide. (Moberly)

Follow Peter T Young on Facebook 

Follow Peter T Young on Google+ 

Follow Peter T Young on LinkedIn  

Follow Peter T Young on Blogger

© 2018 Hoʻokuleana LLC

Koolau_Range-Kaneohe
Koolau_Range-Kaneohe
Koolau Range-Kaneohe Bay-Mokapu
Koolau Range-Kaneohe Bay-Mokapu
Koolau_Range
Koolau_Range
Koolau_Range-Waimanalo
Koolau_Range-Waimanalo
Koolau_Mountains_from_Wahiawa_by_Helen_Thomas_Dranga
Koolau_Mountains_from_Wahiawa_by_Helen_Thomas_Dranga
Tradewinds and the Koolau-Jokiel
Tradewinds and the Koolau-Jokiel
Mokolii lava flows-Jokiel
Mokolii lava flows-Jokiel
Koolau_Caldera-Aerial_Image_(UH_Manoa-Rowland_&_Garcia)
Koolau_Caldera-Aerial_Image_(UH_Manoa-Rowland_&_Garcia)
Koolau Caldera-OregonState
Koolau Caldera-OregonState
Kawainui-200-years_ago_(State_Parks)
Kawainui-200-years_ago_(State_Parks)
Kawainui-6,000-years_ago_(State_Parks)
Kawainui-6,000-years_ago_(State_Parks)
Nuuanu Avalanche-Jokiel
Nuuanu Avalanche-Jokiel
Koolau_Caldera-Map_(UH_Manoa-Rowland_&_Garcia)
Koolau_Caldera-Map_(UH_Manoa-Rowland_&_Garcia)
Nuuanu Avalanche-tamu
Nuuanu Avalanche-tamu
Young and Present-Koolau Caldera-SOEST
Young and Present-Koolau Caldera-SOEST
Oahu-Waianae-Koolau-Caldera-SOEST
Oahu-Waianae-Koolau-Caldera-SOEST

Filed Under: General, Place Names Tagged With: Hawaii, Oahu, Koolau, Koolaupoko, Waianae, Nuuanu Avalanche

October 19, 2018 by Peter T Young Leave a Comment

Waikīkī Beach Agreements

Waikīkī Beach was eroding.

As early as 1901, both the government surveyor and Lili‘uokalani had residences at Waikīkī Beach with walls across their seaward frontages that were in the ocean, blocking public passage along the beach.

Another Waikīkī residence and the Moana Hotel also had portions of their structures similarly situated in the water. By the late-1920s, walls were common along Waikīkī Beach.

A 1927 report by the Engineering Association of Hawai‘i pinpointed seawalls as the primary cause of erosion in Waikīkī. The report concluded that beach nourishment and groins could be used to rebuild the beach.

During the same time period, plans were underway to turn Waikīkī district wetlands into an urban community. The Ala Wai Canal was dredged from 1922 to 1928.

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.

On October 19, 1928, property owners at Waikīkī signed the Waikīkī Beach Reclamation Agreement between the Territory of Hawai‘i and Property Owners – an agreement with the Territory of Hawai‘i to not build any obstructions on what would become Waikīkī Beach.

The agreement was to “forever thereafter keep the beach free and clear of obstructions and open for the use of the public as a bathing beach and for passing over and along the same on foot.”

The Beach Agreement illustrated the need to control and limit seaward development on Waikīkī Beach. The agreement establishes limitations on construction along the beach in response to the proliferation of seawalls and groins in Waikīkī.

The 1928 agreement consists of a) the October 19, 1928 main agreement between the Territory and Waikīkī landowners, b) the October 19, 1928 main agreement between the Territory and the Estate of Bernice Pauahi Bishop and c) The July 5, 1929 Supplemental Agreement between the Territory and Waikīkī landowners.

The agreement provides that the Territory was to use “best efforts” to construct beach area 180-feet seaward for the purpose of beach erosion control together with “maintenance, preservation and restoration thereof as may be necessary from time to time.”

The expanded beach would “be deemed to be natural accretion attached to the abutting property, and title there to shall immediately vest in the owner or owners of the property abutting thereon in proportion to their sea-frontage, subject only to the easement in favor of the public as above stated.”

The private landowners agreed they “will not erect or place on any part of such beach so to be constructed as aforesaid within seventy-five (75) feet of mean highwater mark of such beach as it may exist from time to time …”

“… any building, fence, wall or other structure or obstruction of any kind unless such mean highwater mark shall be more than seventy-five (75) feet from the present line of mean highwater mark.”

The agreement covers the Waikīkī beach area including the area from the Ala Wai Canal to the Elks Club at Diamond Head. The Waikīkī Beach Reclamation Agreement of 1928 gave property owners title to beach fronting their seawalls.

According to the 1928 Waikīkī Beach Reclamation Agreement, no commercial activities are permitted to take place on Waikīkī Beach. All commercial activities originate from private property and people traverse the beach to gain access to the water.

As part of the 1928 Beach Agreement, eleven groins composed of hollow tongue and concrete blocks were built along Waikīkī Beach with the intent of capturing sand. (SOEST)

A lot of the sand to build the beach was brought in to Waikīkī Beach, via ship and barge, from Manhattan Beach, California in the 1920s and 1930s.

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.

In addition, the segment between the Royal Hawaiian Hotel and the Moana Surfrider (Surfrider-Royal Hawaiian Sector Beach Agreement) is the subject of a separate agreement between the Territory and the subject Waikīkī landowners entered into on May 28, 1965.

State law states that the right of access to Hawai‘i’s shorelines includes the right of transit along the shorelines. (HRS §115-4)

The right of transit along the shoreline exists below (seaward of) the private property line (generally referred to as the “upper reaches of the wash of waves, usually evidenced by the edge of vegetation or by the debris left by the wash of waves.”) (HRS §115-5)

Waikīkī Beach is unique because the State does not own all of the land in front of the Royal Hawaiian, Outrigger Waikīkī and Moana Surfrider hotels.

The 1965 agreement between the State and the hotel landowners gave the owners of the abutting hotels 75-feet of the beach in exchange for cooperation with the State’s proposal to extend Waikīkī Beach up to 120 feet from the existing shoreline.

The abutting private beach land is subject to a 75-foot public right of way for the public to pass along the Beach, sunbathe or do other beach activities. The easement in favor of the public restricts commercial activities in the right-of way.

According to the agreement, the State is responsible for maintaining and policing the easement. This easement would be extinguished upon the State building 75-feet of beach seaward of the existing beach, but since that has never happened, the easement remains in effect. (DLNR)

Follow Peter T Young on Facebook 

Follow Peter T Young on Google+ 

Follow Peter T Young on LinkedIn  

Follow Peter T Young on Blogger

© 2018 Hoʻokuleana LLC

Waikiki-Moana_Hotel-1920
Waikiki-Moana_Hotel-1920
Waikiki-fronting_old-Seaside_Hotel-seawall-1915
Waikiki-fronting_old-Seaside_Hotel-seawall-1915
Royal_Hawaiian-rice-taro-duck_ponds-in-background-1929
Royal_Hawaiian-rice-taro-duck_ponds-in-background-1929
Royal_Hawaiian_Hotel-Aerial-December 5, 1928
Royal_Hawaiian_Hotel-Aerial-December 5, 1928
Moana_Hotel-Aerial-1929
Moana_Hotel-Aerial-1929
Royal_Hawaiian_oceanside_construction-(HSA-HHF)-1926
Royal_Hawaiian_oceanside_construction-(HSA-HHF)-1926
Seaside_Hotel-noted-(Moana_Hotel-Apuakehau_Stream-marshland_behind)-1920
Seaside_Hotel-noted-(Moana_Hotel-Apuakehau_Stream-marshland_behind)-1920
Waikiki_Beach_Houses_(UH_Manoa)-1924
Waikiki_Beach_Houses_(UH_Manoa)-1924
Natatorium-1928
Natatorium-1928
Honolulu_and_Vicinity-(portion)-(UH_Manoa-Hamilton_Library)-1923
Honolulu_and_Vicinity-(portion)-(UH_Manoa-Hamilton_Library)-1923
USGS_Map-Waikiki-1927
USGS_Map-Waikiki-1927

Filed Under: General, Place Names, Economy Tagged With: Hawaii, Waikiki, Waikiki Beach, Waikiki Beach Reclamation Agreement

October 15, 2018 by Peter T Young Leave a Comment

David Malo’s Grave

In 1823, Malo moved to Lāhainā, Maui where he learned to read and write. Malo soon converted to Christianity and was given the baptismal name of David.

On September 5, 1831, classes at the Mission Seminary at Lahainaluna (later known as Lahainaluna (Upper Lāhainā)) began in thatched huts with 25 Hawaiian young men.

Under the leadership of Reverend Lorrin Andrews, the school was established by the American Board of Commissioners of Foreign Missions “to instruct young men of piety and promising talents”. It is the oldest high school west of the Mississippi River.

When Sheldon Dibble arrived to Hawai‘i in 1836, “connected with the Mission Seminary at Lahainaluna, and being called to teach History as one branch of my department of instruction”.

He had found it “quite objectionable that the scholars, whilst they were becoming acquainted with other nations, should remain to a great degree in ignorance of their own.”

Dibble made an “effort to collect the main facts of Hawaiian history,” he “selected ten of the best scholars of the Seminary, and formed them into a class of inquiry.”

Dibble “requested them to go individually and separately to the oldest and most knowing of the chiefs and people, gain all the information that they could on the question given out, commit each his information to writing and be ready to read it on a day and hour appointed.” (Dibble, April 28, 1843) One of the leading students was Malo.

“(David) Malo was the son of Aoao and his wife Heone, and was born at the seaside town of Keauhou, North Kona, Hawaii, not many miles distant from the historic bay of Kealakeakua, where Captain Cook, only a few years before, had come to his death.”

“The exact year of his birth cannot be fixt’d, but it was about 1793, the period of Vancouver’s second visit to the islands. … During his early life Malo was connected with the high chief Kuakini (Governor Adams), who was a brother of Queen Kaahumanu …”

“… and it was during this period specially that he was placed in an environment the most favorable to forming an intimate acquaintance with the history, traditions, legends and myths of old Hawaii, as well as with the meles, pules and olis that belong to the hula and that form so important and prominent a feature in the poesy and unwritten literature of Hawaii.”

“Such good use did Malo make of his opportunities that he came to be universally regarded as the great authority and repository of Hawaiian lore.” (NB Emerson)

Malo was ordained into the Christian ministry and settled down in the seaside village of Kalepolepo on East Maui. (Trinity) His book, Hawaiian antiquities (Moolelo Hawaii – 1898,) addressed the genealogies, traditions and beliefs of the people of Hawai‘i.

In the “Narrative of the United States Exploring Expedition,” Admiral Wilkes (1840,) commenting on books about Hawai‘i, said, “(s)ome of them are by native authors. Of these I cannot pass at least one without naming him.”

“This is David Malo, who is highly esteemed by all who know him, and who lends the missionaries his aid, in mind as well as example, in ameliorating the condition of his people and checking licentiousness.”

“(A)s Malo aged, and perhaps because he spent so much time pondering the old traditions in writing Hawaiian Antiquities or wading through Lahaina’s crowds of seamen on leave, he became increasingly exasperated with the rising tide of haoles as the Hawaiians died and kept on dying.”

“In a letter to native friends, he wrote: If a big wave comes in, large and unfamiliar fishes will come from the dark ocean, and when they see the small fishes of the shallows they will eat them up.”

“The white man’s ships have arrived with clever men from the big countries. They know our people are few in number and our country is small, they will devour us.” (Malo; Vowel)

Malo died October 21, 1853. “The death of the well-known native preacher, David Malo, is one of those events which throw sorrow upon the hearts of the friends of the native race.”

“Seeing a white object on the very summit of Mt. Ball (a hill above Lahainaluna School), a day or two since, I inquired what it was.”

“It was David Malo’s tomb. And why was he buried in so strange spot? He wished it. He said this land would fall into the possession of foreigners.”

“Land in Lahaina would be valuable. The graveyards, enriched by the remains of the natives, would be coveted, and the contents of the graves scattered abroad.”

“He wished not his bones to be disturbed. Let him be buried on that summit where no white man will ever build his house.”

“And so his grave has become beacon; and if his spirit ever lingers over it, he can survey, as from lofty watch-tower, his former home, and the scene of many of his labors.” (Sereno Bishop; The Friend, November 16, 1853)

Malo’s grave is on Pu‘u Pa‘upa‘u (sometimes called Mt Ball) – that is the hill above Lahaina with the ‘L’ (standing for Lahainaluna, the school that Malo attended).

Follow Peter T Young on Facebook 

Follow Peter T Young on Google+ 

Follow Peter T Young on LinkedIn  

Follow Peter T Young on Blogger

© 2018 Hoʻokuleana LLC

David Malo grave
David Malo grave
David Malo grave
David Malo grave
54-David_Malo

Filed Under: Missionaries / Churches / Religious Buildings, Place Names, Prominent People Tagged With: Mr Ball, Lahainaluna, David Malo, Lahaina, Puu Paupau

October 13, 2018 by Peter T Young 1 Comment

Moʻomomi

Kaumaha i ka naulu Kaluakoi.
Laden with the summer showers is Kaluakoi.
(Kaluakoi gets rain only in the summer time.) (McElroy)

Kaluakoʻi is the largest ahupuaʻa, or land division, on the island of Molokai. With regard to ahupuaʻa, Lyons asserts that, “in populous portions the sub-division was very minute” (1875.)

Consequently, the size of the Kaluakoʻi ahupuaʻa would suggest a small population for this part of Molokai, a situation borne out by the archaeological record.

The ahupuaʻa of Kaluakoʻi literally means, the “the adze pit.” In this ahupuaʻa, high quality basalt was used to make adzes and other tools. It is well known that lithic quarries occurred on select sites in the area, notably on the summit of Maunaloa at ʻAmikopala, and on northwest Molokai at Moʻomomi and ʻIlio Point. (McElroy)

West Molokai is roughly two million years old and its long dormancy has allowed a deep lateritic soil to develop that covers most of the region. “The Desert Strip,” was coined by Chester Wentworth, who described this extensive dune system as a “barren windswept country in which eolian features are developed with exceptional clarity and vigor”.

The dominant northeast trade winds have blown sand from Moʻomomi almost completely across the northwest corner of the island creating an expansive stretch of sand dunes. The Hawaiians called this same area Keonelele, or “the flying sand.”

The main part of the Moʻomomi Dunes probably was formed during the latest ice age, when sea level was low and the reefs now submerged offshore were dry and feeding sand into the wind. Since then, slightly acidic rain has cemented some of the sand into hard limestone. (McElroy)

A recent study found that 40% of Molokai families’ food came from subsistence activities. The Hoʻolehua Hawaiian Homestead community on Molokai relies heavily for subsistence on the inshore marine resources of the Moʻomomi fishery, which falls within a twelve-mile stretch of coastline along Molokai’s north shore. (Kohala Center)

Coastal fisheries are facing severe depletion and overexploitation on a global scale and Hawai‘i is no exception.

Hui Malama o Moʻomomi cares for the land and nearshore waters along the Moʻomomi Coast on the island of Molokai. Protection of this place is to assure a reliable food source; as the community is very much subsistence-based, the ocean is their “ice box.”

Co-founder of the Hui Malama o Moʻomomi, Mac Poepoe, led the way toward educating others about the coastal resources found in Moʻomomi Bay and pono (proper) behaviors that ensure not only familial but community subsistence.

Poepoe established Hui Mālama o Moʻomomi in 1993 in order to teach younger generations the ancient practices of traditional Hawaiian fishing and how to become responsible marine citizens.

It is a local marine subsistence/sustainability grassroots organization, assisting with management on the state’s Hawaiian Homelands. The Hui oversees marine subsistence gathering and sustainability practices.

Important management lessons to learn from this are to recognize natural rhythms, do not disturb basic renewal processes, monitor (moon, season, habitat, etc) and understand the resource. As a foundation to this, we need to recognize the interconnected link between the land and the ocean.

Community-based management in the Mo‘omomi area involves observational processes and problem-solving strategies for the purpose of conservation. The system is not articulated in the manner of Western science, but relies instead on mental models.

These models foster a practical understanding of local inshore resource dynamics by the fishing community and, thus, lend credibility to unwritten standards for fishing conduct. The “code of conduct” is concerned with how people fish rather than how much they catch. (Poepoe)

Through Poepoe’s efforts, almost single-handedly, they rejuvenated Moʻomomi Beach by controlling erosion, reintroduced native plants and monitored fish populations. The beach is now rich with vegetation, and the moi are as big as small-kid time. (Cooke)

A code of conduct on appropriate behavior was designed to be true to Hawaiian values, to consider the community’s culture and be biologically sound for resource sustainability.
• Rule 1 – Take only what you need. Share your catch with others.
• Rule 2 – Reserve inshore areas for children and novice swimmers and fishermen.
• Rule 3 – Education. Utilize traditional practices and science-based methods.
• Rule 4 – Community governing board.
• Rule 5 – Malama. Care for the land; care for the people; care for all things; understand the land with the ocean.

Community members are joining with state officials to develop a designation for Molokai’s north shoreline that would sustainably support marine resources, protect traditional fishing practices, prohibit commercial harvest and facilitate community involvement in resource management decisions. (Molokai Dispatch)

The group is looking to organize a Community-based Subsistence Fishing Area along the Northwest Coast of Molokai, including Moʻomomi.

Nearby land-based management is underway through The Nature Conservancy (TNC.) Mo‘omomi Preserve was established in June of 1988 to protect the most intact coastal sand dune ecosystem in the main Hawaiian Islands.

The westernmost coastline of the preserve is characterized by sea cliffs; the remainder of the two‐mile long coastline consists of windswept sand beaches, and dunes.

The upper dune area of the preserve is known as Keonelele, “the flying sands”. Portions of the preserve dunes are lithified (sand dunes that become solidified) and are distinct in geological appearance and native strand. (TNC)

Moʻomomi is a nesting location for wedge-tailed shearwater seabirds, or ʻuaʻu kani in Hawaiian. TNC is taking an active role in protecting these ground-nesting birds from feral cats and dogs, as well as promoting scientific study.

Moʻomomi is a breeding and nesting area for the Hawaiian green sea turtle, or honu in Hawaiian, and they are actively monitored by TNC staff and volunteers. It is believed that the females return to lay eggs on the same beach where she was hatched and may live as long as 100 years, though its life span is not known for sure. (McElroy)

Follow Peter T Young on Facebook 

Follow Peter T Young on Google+ 

Follow Peter T Young on LinkedIn  

Follow Peter T Young on Blogger

© 2018 Hoʻokuleana LLC

Moomomi-Rogers
Moomomi-Rogers
Hui_Malama_o_Mo'omomi_by_MolokaiPhotography
Hui_Malama_o_Mo’omomi_by_MolokaiPhotography
moomomi-beach
moomomi-beach
Cave at Moomomi Preserve, Molokai
Cave at Moomomi Preserve, Molokai
Moomomi TickleMePick
Moomomi TickleMePick
Kawa’aloa Beach Mo’omomi Moloka’i-kyle
Kawa’aloa Beach Mo’omomi Moloka’i-kyle
Moomomi_Dunes-TickleMePick
Moomomi_Dunes-TickleMePick
Moomomi_TickleMePick
Moomomi_TickleMePick
Moomomi
Moomomi
Moomomi-TickleMePick
Moomomi-TickleMePick
Land_Office_Map_of_the_Island_of_Molokai,_Hawaii_-_Geographicus_-_1897-portion-Kaluakoi-W_Molokai
Land_Office_Map_of_the_Island_of_Molokai,_Hawaii_-_Geographicus_-_1897-portion-Kaluakoi-W_Molokai
1897_Land_Office_Map_of_the_Island_of_Molokai,_Hawaii_-_Geographicus_-_1897
1897_Land_Office_Map_of_the_Island_of_Molokai,_Hawaii_-_Geographicus_-_1897

Filed Under: General, Hawaiian Traditions, Place Names Tagged With: Molokai, Kaluakoi, Moomomi, Mac Poepoe, Hawaii

  • « Previous Page
  • 1
  • …
  • 107
  • 108
  • 109
  • 110
  • 111
  • …
  • 154
  • Next Page »

Images of Old Hawaiʻi

People, places, and events in Hawaiʻi’s past come alive through text and media in “Images of Old Hawaiʻi.” These posts are informal historic summaries presented for personal, non-commercial, and educational purposes.

Info@Hookuleana.com

Connect with Us

  • Email
  • Facebook
  • LinkedIn
  • Twitter
  • YouTube

Recent Posts

  • ‘Aim High to Reach the Heaven’
  • Presidents’ Day
  • Moku Manu
  • Valentine’s Day
  • Louis Henri Jean Charlot
  • Greek Artillery
  • Land Divisions

Categories

  • Place Names
  • Prominent People
  • Schools
  • Sailing, Shipping & Shipwrecks
  • Economy
  • Voyage of the Thaddeus
  • Mayflower Summaries
  • American Revolution
  • General
  • Ali'i / Chiefs / Governance
  • Buildings
  • Missionaries / Churches / Religious Buildings
  • Hawaiian Traditions
  • Military

Tags

Albatross Al Capone Ane Keohokalole Archibald Campbell Bernice Pauahi Bishop Charles Reed Bishop Downtown Honolulu Eruption Founder's Day George Patton Great Wall of Kuakini Green Sea Turtle Hawaii Hawaii Island Hermes Hilo Holoikauaua Honolulu Isaac Davis James Robinson Kamae Kamaeokalani Kameeiamoku Kamehameha Schools Lalani Village Lava Flow Lelia Byrd Liberty Ship Liliuokalani Mao Math Mauna Loa Midway Monk Seal Northwestern Hawaiian Islands Oahu Papahanaumokuakea Marine National Monument Pearl Pualani Mossman Quartette Thomas Jaggar Volcano Waikiki Wake Wisdom

Hoʻokuleana LLC

Hoʻokuleana LLC is a Planning and Consulting firm assisting property owners with Land Use Planning efforts, including Environmental Review, Entitlement Process, Permitting, Community Outreach, etc. We are uniquely positioned to assist you in a variety of needs.

Info@Hookuleana.com

Copyright © 2012-2024 Peter T Young, Hoʻokuleana LLC

 

Loading Comments...