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December 16, 2024 by Peter T Young Leave a Comment

Kona

“The story of the Polynesians began about 6,000 years ago when a seafaring people traveled from Asia or Melanesia to the islands of Samoa and Tonga. Their descendants eventually sailed east to Tahiti and the Marquesas Islands.  Later they sailed south to New Zealand, east to Easter Island, and north to the Hawaiian Islands.”

“By A.D. 1200, the ancient Polynesians voyagers had settled nearly every habitable island over some ten million square miles of the Pacific Ocean.” (Hawaiian Encyclopedia A Comprehensive Guide To The Hawaiian Islands History, Culture, Native Species, Science)

“Polynesian is part of a subgroup of Austronesian called Oceanic which includes all the Austronesian languages of Polynesia, Island Melanesia, coastal New Guinea east of 136 degrees East longitude, and Micronesian languages other than two Western Micronesian languages: Chamorro (Mariana Islands) and Belauan (Belau, formerly Palau).”

“[I]t is clear that Proto Polynesian speech and culture (ca. 1-300 A.D.) was a product of something like 1000 years of development in fair isolation from the outside world. ‘Polynesian’ language and culture did not arrive fully formed in Polynesia.”

“The language and culture of the early Oceanic Austronesian speaking settlers who gave rise to the modern cultures we observe in Polynesia were greatly transformed in Polynesia itself before internal diversification became pronounced.”

“‘Polynesian; language and culture ‘came from’ the west as most people have long imagined, but it wasn’t Polynesian when it arrived. It became Polynesian in situ, differentiating from a linguistic and cultural base originating in Insular Southeast Asia and initially transformed as it spread across Melanesia towards Polynesia over a period of hundreds of years.” (Jeff Marck)

“Sikaiana legends record an invasion from ‘Tona’ about 12-14 generations ago in their genealogies (from the 1980s). They associate Tona with Tonga, although Tona is a common Polynesian word for “south” and many Western Polynesian societies have similar legends of people from the ‘south.’” (Kutztown University)

“The people of Tonga (correctly pronounced tona, as in ‘Kona’, Hawaii) met Captain Cook with such warm greetings that he called the islands of Tonga the ‘Friendly Islands’”. (NOAA)

“’[T]onga’ means ‘south’ in the Tongan language and refers to the country’s geographic position in relation to central Polynesia”. (CIA)

Dictionaries state, “Hawaiian Dictionary – Kona 1. nvs. Leeward sides of the Hawaiian Islands; leeward (PPN [Proto-Polynesian language] Tonga.)

“[Parker Dictionary (Hawaiian)] Kona (kō’-na), n. 1. South (opposite of koolau, which is north). 2. The southwest wind; also the south wind. 3. The rain accompanying a south wind: He ua kona, he ua nui loa ia; a kona rain is a very great rain.  4. The south or southwest sides of the Hawaiian islands.”

“In all probability, Tonga and Tona or Kona, the name of a district … of Hawaii, are one and the same word; and, to give an instance of which there can be no doubt, tangata, the Samoan for man, has been softened into the Hawaiian tanata or Kanaka.” (Sir George Simpson, An Overland Journey Round the World (1841-1842))

“Explorers are not new to the Kingdom of Tonga (Pule’anga Fakatu’i ‘o Tonga), an archipelago of 176 islands south of Samoa in the South Pacific Ocean. The Dutch were some of the earliest explorers to arrive on the island in the 17th century, followed by other Europeans, including Captain James Cook of the British Navy.”

“As a word, ‘Kona’ is often translated as ‘leeward’. But the full meaning invites explication.  The word is of ancient origin and exists across the Austronesian language family in other forms.  For example, further south it is spoken as ‘tonga’. And thus the name of the South Pacific island chain and Nation.”

“What kona land areas are leeward of is the direction of the trade winds. Within the Hawaiian island chain, four of the six major islands contain district names Kona by original Hawaiian settlers.”

“The indigenous geographic concept of kona is more than simply a directional relationship. Kona districts have particular environments created by the specific microclimates that exist from being leeward.” (Jolliffe)

“The expressions Tonga, Kona, Toa (Sam., Haw., Tah.), to indicate the quarter of an island or of the wind, between the south and west, and Tokelau, Toerau, Koolau (Sam., Tah., Haw.), to indicate the opposite directions from north to east …”

“… expressions universal throughout Polynesia, and but little modified by subsequent local circumstances point strongly to a former habitat in lands where the regular monsoons prevailed.”

“Etymologically ‘Tonga,’ ‘Kona,’ contracted from ‘To-anga’ or ‘Ko-ana,’ signifies ‘the setting,’ seil. of the sun. ‘Toke-lau,’ of which the other forms are merely dialectical variations, signifies ‘the cold, chilly sea.’” (Fornander I)

“Mr. Hale, in the Ethnological portion of the United States Exploring Expedition under Commodore Wilkes, considers the application of Tonga to the south-western quarter as subsequent to the dispersion of the Polynesians in the Pacific (vid. p. 180).”

“But Mr. Hale, in the very same article, has very lucidly shown that ‘Tonga’ was a term applied to the very first settlement of the Polynesians in the Pacific, on Viti-Iewu, signifying ‘the Western,’ seil. people, in contradistinction from the Viti proper, or ‘Eastern’ people.”

“Hence it is reasonable to infer that the Polynesians brought the term with them as an already existing appellation of the western quarter, as much so as they did the other term of ‘Toke-lau,’ to designate the eastern quarter. (Fornander I)

© 2024 Ho‘okuleana LLC

Filed Under: Place Names, General, Hawaiian Traditions Tagged With: Hawaii, Kona, Koolau, Tonga, Leeward

November 21, 2024 by Peter T Young Leave a Comment

It’s Raining … Inside

The Koʻolaupoko moku (district) encompasses lands from Kualoa Point to Makapuʻu Point. Encompassing 43,598-acres (68-square miles,) Koʻolaupoko makes up approximately 11-percent of Oʻahu’s land mass.

The Koʻolau Mountain Range forms the inland (mauka) boundary of the district. The ridge elevation generally ranges from 2,500 to 2,800-feet; Kōnāhuanui, the tallest peak on the Koʻolau Mountain Range (3,150-feet) is found in Koʻolaupoko. (BWS)

Koʻolaupoko is the remnant of the Koʻolau volcano. Eruptions forming the mountains occurred approximately 2-million years ago and left lava flows that layered over each other.  Magma pouring out of fissures in the volcano solidified in the narrow cracks; the rock that is created is much denser and much less permeable than the surrounding porous lava flows.

These dense, usually vertical geological structures are known as volcanic dikes. These dikes form wall-like areas that can capture and contain water.

Trade winds, which blow over the Pacific from the northeast across the Hawaiian Islands, bring large quantities of moist air to the Koʻolau Range. When these winds are deflected up and over the range, the water vapor condenses into clouds and falls as rain.

The rainfall does one of three things: (1) it runs off, eroding the land, forming valleys and gouges in the mountain slopes (and also creates some spectacular periodic waterfalls;) (2) wets the land surface, shallow infiltration saturates the uppermost soil layer and replaces soil moisture used by plants and then is absorbed by the vegetation and/or evaporates (evapotranspiration;) or (3) it percolates into the ground (slowly sinks into the ground and becomes groundwater.)

For the latter, it takes about 9-months for the rain, now groundwater, to seep down through cracks and permeable materials in the mountain; much of the groundwater ends up contained in dikes inside the mountain.

As these dike compartments become filled with water and overflow the dike edges, sometimes the water emerges at the surface as springs or streams.

Dike water is good for drinking water.

Development of dike-impounded reservoirs for domestic water offers two basic benefits: (1) the water level is typically high (limiting pumping (as in energy to pump water up wells) and allowing gravity to distribute to the needs at lower elevations) and (2)  the reservoirs are isolated from saline water.

Groundwater impounded by dikes in the Koʻolau Range is a major source of water for the island of Oʻahu, and many tunnels have been bored into the range to develop it. (USGS)

The typical sequence of excavation of a high-altitude tunnel starts with the removal of a zone of weathered rocks, either by tunneling or trenching and is followed by penetration of dike intrusions in the basalt rock.

As tunneling advances farther and farther through the dikes and basalts, the contained dike water leaks and water flow increases, often in instantaneous jumps when key restraining dikes are punctured, until either a single dike, or a series of them, releases such a large volume of stored water that excavation must be halted.  (Mink; USGS)

When a tunnel is bored into a dike-water reservoir, if allowed to flow freely, it will drain water out of storage. Over the course of water exploration in this area, several dikes were struck.

The reduction of dike-confined groundwater storage caused by construction of eight tunnels in Oʻahu has been estimated at 25,800-Million gallons, equivalent, then, to the total ground-water withdrawal on Oʻahu for about 60 days.   (USGS)

Little consideration was given to the storage potential of dike compartments tapped and dewatered by water-development tunnels until a bulkhead was placed in a Waikāne tunnel of the Waiāhole system in 1934 to stop the draining and allow the dike to refill with water (about 40 years after high-altitude water-development tunnels were first constructed in Hawaiʻi.)

The bulkhead at Waikāne held back some water in storage, but not in sufficient volume to be considered successful. Use of the Waikāne bulkhead was discontinued, but other attempts at bulkheading were tried elsewhere, also without much success.

That changed on February 8, 1955.  A 12-foot dike 1,600 feet into the Waiheʻe tunnel was penetrated and water gushed out at an initial rate of about 2.5-mgd (million gallons per day.)   A bulkhead was built to contain the water.

The bulkhead held and the concept of inducing and controlling storage was resoundingly proved with the placement of the bulkhead in Waiheʻe tunnel.  The storage above the tunnel in Waiheʻe Valley has been estimated at 2,200-Million gallons.  (Mink; USGS)

In Koʻolaupoko, fresh water comes entirely from precipitation along the Koʻolau Mountain Range; Waiheʻe provides much of the drinking water to Windward Oʻahu, from Kahaluʻu to Kailua.

The Honolulu Board of Water Supply recently drilled an inclined well to tap dike-impounded water. This technique permitted the development of dike impounded water without the large initial and uncontrollable waste of stored water common to prior development by tunneling.

Dike tunnel systems are also at Waimānalo, Luluku, Haiku, Kahaluʻu, Pālolo, Mānoa and two Waianae tunnels, as well as in the Kohala region of the island of Hawaiʻi and in West Maui.

Oh, It’s Raining … Inside (?)

While the bulkhead holds the dike water, along the Waiheʻe tunnel into the Koʻolau, whatever the weather outside, rainwater (now groundwater) that missed the dike continues to make its downward percolation through the mountain, through cracks in the ceiling … producing a constant ‘rainfall’ for all in the darkness of the tunnel to the Waiheʻe bulkhead.

© 2024 Hoʻokuleana LLC

Filed Under: General, Place Names, Economy Tagged With: Hawaii, Oahu, Koolau, Koolaupoko, Waihee

March 25, 2022 by Peter T Young Leave a Comment

Keʻanae Prison Camp

In June, 1925, Governor Wallace Farrington and the County Board of Supervisors Chairman Samuel Kalama led a grand procession of cars on the official opening of the road from Kailua to Hana.

The road was called the Belt Road and would link the isolated communities of East Maui with the rest of the island. By December, 1926, the governor and the board chairman were able to drive all the way to Hana on the dream road that was fast becoming a reality.

Wait … Let’s step back a bit.

Handy, Handy & Pukui report that in ancient times there were several major population centers on the Island of Maui: Kahakuloa (West Maui) region; the deep watered valleys of Nā Wai ‘Ehā (Waiheʻe, Wai‘ehu, Wailuku and Waikapū;) the ‘Olowalu to Honokōhau region of Lāhainā; the Kula – ʻUlupalakua region and the Koʻolau – Hāna region.

They note the importance of the Koʻolau region in this discussion: “On the northeast flank of the great volcanic dome of Haleakala…the two adjacent areas of Keʻanae and Wailua-nui comprise the fourth of the main Maui centers and the chief center on this rugged eastern coast”

“It supported intensive and extensive wet-taro cultivation. Further eastward and southward along this windward coast line is the district of Hāna…” (Maly)

Settlement in the watered valleys along the Koʻolau coast consisted primarily of permanent residences near the shore and spread along the valley floors. Residences also extended inland on flat lands and plateaus, with temporary shelters in the upper valleys.

Handy, Handy and Pukui further note that “…Ke‘anae lies just beyond Honomanu Valley. This is a unique wet-taro growing ahupua‘a… It was here that the early inhabitants settled, planting upland rain-watered taro far up into the forested area.”

“In the lower part of the valley, which is covered mostly by grass now, an area of irrigated taro was developed on the east side. A much larger area in the remainder of the valley could have been so developed.”

“However, we could find no evidence of terracing there. This probably was due to the fact that the energies of the people were diverted to create the lo‘i complex which now covers the peninsula.” (Maly)

In modern times, when Hāna was without a road, and the coastal steamer arrived on a weekly schedule, Hana-bound travelers unwilling to wait for the boat drove their car to the road’s end at Kailua, rode horseback to Kaumahina ridge, then walked down the switchback into Honomanu Valley. (Wenkam, NPS)

Friends carried them on flatbed taro trucks across the Keʻanae peninsula to Wailua cove. It was a short ride by outrigger canoe beyond Wailua to Nāhiku landing where they could borrow a car for the rest of the involved trip to Hana. Sometimes the itinerary could be completed in a day. Bad weather could make it last a week. (Wenkam, NPS)

It was not until 1847, that the historic and modified trail and road alignments became a part of a system of “roads” called the “Alanui Aupuni” or Government Roads. Work on the roads was funded in part by government appropriations, and through the labor or financial contributions of area residents, or prisoners working off penalties. (Maly)

The law (Sec 1536DD. Warden, Deputy, Duties, Powers) allowed a warden to have “the immediate charge and direction of all Territorial prisons and prison camps and the administration thereof.”

“The warden shall be responsible for the safekeeping of all prisoners and persons who may be committed to said prisons and for the enforcement of proper order and discipline among and concerning prisoners and prison officers and employees.” (Attorney General)

Neighbor Island prison camps were set up, there were 4: Maui had three, the other was on the Big Island (outside Hilo.) Keʻanae camp had 22-prisoners and 3-guards; Olinda camp had 31-prisoners, with Jailer and 3-guards and Paukakulo camp had 27-prisoners, with 1-jailer and 3-guards. The three camps on Maui are engaged in road work and forest lines.

A large part of the road to Hāna was constructed by prison labor based at the Keʻanae Prison Camp. The camp was built in 1926 to house the prisoners who would construct the road, including several bridges from Kailua to Hana.

When the road was completed in 1927, men from Keʻanae to Hāna town were hired to maintain the road, especially during the rainy season. (McGregor)

Later, an announcement in the Maui News (January 20, 1934) carried the headline, “Conservation Program Will Be Launched Within Week or 10 Days.” Sub-headlines were “$421,000 Is Provided” and “…To be Located at Keʻanae’s Old Prison Site.”

No longer needed, the Keʻanae prison camp was converted into quarters for the Civilian Conservation Corps. This federal program, created by President Franklin D. Roosevelt to provide jobs to get the US through the depression, brought in men from other parts of Maui and other islands to plant thousands of eucalyptus and other introduced trees throughout the Hana coast. (McGregor)

In December 1942, during World War II, Governor Ingram Stainback tried to assist the war effort by sending forty inmates from Oʻahu Prison to the former Keʻanae Prison camp to revive the old Nāhiku rubber plantations in the hope of yielding 20,000 to 50,000-pounds of crude rubber annually. The venture was no more successful than the earlier ones had been.

Eventually, the YMCA operated the facilities as Camp Keanae; part of the land area continues to be used as a roadway base yard. Na Moku Aupuni O Ko‘olau Hui are now the stewards of Camp Keanae.

© 2013 Hoʻokuleana LLC

 

Filed Under: Economy, General, Place Names Tagged With: Hawaii, Maui, Koolau, Hana, Keanae, Keanae Prison, Hana Highway

February 4, 2022 by Peter T Young Leave a Comment

Built in About an Hour

The Hawaiian Islands were formed as the Pacific Plate moved westward over a geologic hot spot.  Oʻahu is dominated by two large shield volcanoes, Waiʻanae and Koʻolau that range in age from two to four-million years old.

The younger volcanic craters are all less than 500,000 years old. They formed after Oʻahu had moved well off the hot spot and the main shield volcanoes had gone dormant for at least two-million years.

Scientists say Lēʻahi (Diamond Head) (one of these later eruptions) is a tuff cone, formed by hydromagmatic activity.  Tuff is a volcanic rock made up of a mixture of volcanic rock and mineral fragments. Wherever there are explosive volcanic eruptions you can expect to find tuff.  (SOEST)

A hundred years ago, Hawaiʻi missionary Reverend Sereno Bishop noted Diamond Head was made in less than an hour’s time and is “composed not of lava, like the main mountain mass inland, but of this soft brown rock called tuff.” (Bishop, Commercial Advertiser, July 15, 1901)

Others noted, “the duration of eruption of Diamond Head was of the order of five hours. The eruption may have been intermittent with interruptions sufficient to extend the whole period of activity to as much as five days, but probably not more.”    (Wentworth, Bishop Museum, 1926)

“Volcanic eruptions may be distinguished into two classes, the effusive and the explosive. In the former the molten rock is poured out and covers the mountain slopes with great floods.”

“If you look up at the sides of yonder ravines (on the Koʻolau mountains,) which the rainstorms of many hundred thousands of years have worn out of the original dome-shaped mountain, you will see the back edges of the ancient lava streams lying in layers.”

“The tuff cones are entirely different, and are produced by very brief and sudden explosive eruptions.  The tuff was violently shot high aloft into the air in the form of superheated mud. This hot mud cooled and thickened by the expansion of its water and its partial escape as steam before reaching the ground.”

“It hardened and cemented as it fell, though still liquid enough to form in thin layers or laminations as we see it lying around us at the base of the hill. … The tuff-fountain escaping from its confinement, at once expanded and spread out like a vast tree.”

“Here at Diamond Head, which is one mile in diameter, the bulk of the mud spread out half a mile in all directions before ending its fall. Thus a very exact circular ring was piled up of one mile in diameter. There was, however, another influence, that of a violent easterly-wind which deflected the entire fountain westward”.

“The wind also acted with especial force upon the highest part of the fountain, flinging and piling it up on the western side of the crater in a lofty cone. A large part of that cone has been weathered away by the impact of rainstorms upon the soft rock; but it still stands in a peak some 200 feet higher than the main run.”

“The vent or point of issue of the tuff-fountain must have been at the lowest point of the interior, where lies the present pond of water.”  (Bishop, Commercial Advertiser, July 15, 1901)  (The same series of eruptions produced Punchbowl and Koko Head Crater.)

Somewhat more than half of the craters of southeast Oahu are arranged in linear groups, those dominated by the craters Tantalus, Diamond Head, and Koko Crater.  In the Diamond Head group is the main Diamond Head vent, Kaimuki crater and Mauʻumae crater.

(A cinder cone is a volcanic cone built almost entirely of loose volcanic fragments called cinders or pumice that accumulate around and downwind from a vent.)

(Cinders are glassy and contain numerous gas bubbles “frozen” into place as magma exploded into the air and then cooled quickly.)  (USGS)

© 2022 Hoʻokuleana LLC

 

Filed Under: General, Place Names Tagged With: Diamond Head, Hawaii, Oahu, Koolau, Sereno Bishop, Leahi

March 26, 2020 by Peter T Young Leave a Comment

Ahupuaʻa ‘Anomalies’

Typically, we think of ahupuaʻa in the general context of the modern day watershed – from the mountains to the sea (ridges to reefs,) affording occupants access to the various climatic and resource zones.

Ahupuaʻa served as a means of managing people and taking care of the people who support them, as well as an easy form of collection of tributes by the chiefs. Ultimately, this helped in preserving resources.

Shaped by island geography, ahupuaʻa varied in shape and size (from as little as 100-acres to more than 100,000-acres.)

Each ahupuaʻa had its own name and boundary lines. Often the markers were natural features such as a large rock or a line of trees or even the home of a certain bird. A valley ahupuaʻa usually used its ridges and peaks as boundaries.

In ancient Hawaiian times, relatives and friends exchanged products. The upland dwellers brought poi, taro and other foods to the shore to give to kinsmen there. The shore dweller gave fish and other seafood. Visits were never made empty-handed but always with something from one’s home to give.

Ahupuaʻa contained nearly all the resources Hawaiians required for survival. Fresh water resources were managed carefully for drinking, bathing and irrigation.

A typical ahupuaʻa was a long strip of land, narrow at its mountain summit, becoming wider as it ran down a valley into the sea to the outer edge of the reef. If there was no reef, then the sea boundary would be one-mile from the shore.

However, there are several ‘anomalies’ to this conventional ahupuaʻa layout.

Some include multiple parts, even skipping over water. Others do not have contact with the ocean, nor reach a mountain peak. Another includes portions of a couple of mountains. Here are some examples (there are others, as well.)

On the island of Hawaiʻi, the ahupuaʻa of Kīʻao in the moku (district) of Kāʻu is land-locked and doesn’t reach the ocean. (Paman) In addition, it doesn’t reach a mountain summit.

Also on the Island of Hawaiʻi, the ahupuaʻa of Humuʻula starts at the summit of Mauna Loa, crosses the saddle between the two mountains and skirts along the side of Mauna Kea and eventually runs down to the ocean along the Hāmākua coast.

This traversing along a relatively similar contour on the side of Mauna Kea is unique; in addition, in doing so, it essentially cuts off the numerous ahupuaʻa along the South Hilo, North Hilo and Hāmākua coasts to the Mauna Kea summit.

Interestingly, the entire island of Kahoʻolawe is part of the Honuaʻula moku (district) across the ocean on Maui. Kahoʻolawe is not its own ahupuaʻa; rather, it is divided into ʻili (smaller land units within ahupua‘a.)

Historically, a “cloud bridge” connected Kahoʻolawe with the slopes of Haleakalā. The Naulu winds brought the Naulu rains that are associated with Kahoʻolawe (a heavy mist and shower of fine rain that would cover the island.)

Heʻeia on the windward side of Oʻahu runs from the mountains to the sea, but also crosses over a portion of the water in Kāneʻohe Bay and includes a portion of a Mōkapu peninsula across the Bay.

The Waiʻanae ahupuaʻa also has an un-typical shape – it is sometimes referred to in two parts: Waiʻanae Kai, on its western side, runs from the ocean to the Waiʻanae Mountains (like a typical ahupuaʻa – this portion of Waiʻanae runs from the mountain to the sea.)

From there, however, the section referred to as Waiʻanae Uka continues across Oʻahu’s central plain and extends up into the Koʻolau Mountains – extending approximately 15-miles from the Waianae Mountains to the Koʻolau Mountains and ends up overlooking the windward coastline. (Each section is within the same ahupuaʻa.)

Waimānalo is another Oʻahu ahupuaʻa that is ‘anomalous’ to the ‘ridges to reefs’ characterization of the ‘typical’ ahupuaʻa.

Waimānalo extends from the ridge behind Keolu Hills, around Makapuʻu and ending at Kuliʻouʻou Ridge (Koʻolaupoko Hawaiian Civic Club;) it essentially wraps over the Koʻolau range from the windward coast to the leeward coast Oʻahu.

Waimānalo incorporates what was once the large fishpond of Maunalua, now known as Hawaiʻi Kai. Kamakau notes, “The ahupuaʻa of Waimānalo, including the fishpond at Maunalua and the travelling uhu of Makapuʻu, belonged to Mauimua (First-Maui.)” (Koʻolaupoko Hawaiian Civic Club)

The image shows a map of the Islands with some of the anomalies to the typical’ ahupuaʻa.

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Typical_Ahupuaa_Layout_and_Land_Uses-(UH-DURP)

Filed Under: Hawaiian Traditions, Place Names Tagged With: Waimanalo, Koolau, Koolaupoko, Kahoolawe, Ahupuaa, Waianae, Honuaula, Humuula, Hawaii

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