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July 18, 2025 by Peter T Young Leave a Comment

Punahou Taro Patch

“Long ago an aged couple dwelled near the present spring. At a time of drought and famine, the people were obliged to search the mountains for ti root and wild yams for food, and to trudge to Kamo‘ili‘ili to fill their calabashes with drinking water.”

“One night the old woman dreamed that a man appeared to her, to whom she complained bitterly about having to go so far for water, whereupon he said: “He wai no” (“There is water”) and told her that beneath the trunk of an old hala tree nearby she would find it.”

“She awoke her husband and told him the dream, but he made light of it. The next night he had a similar dream. The apparition directed him to go to the sea and catch some red fish, to roast them in ti leaves, reserving a part as an offering to the family deities, and then to pull up the old hala tree by the roots.”

“He awoke, and lo! it was a dream. But the impression it made on him was so strong that in the morning he hastened to carry out the directions which he had received, and when at last he pulled up the hala tree, water oozed out from beneath its roots.”

“He dug out the place, and thus formed the spring, which was named Kapunahou. A pond was formed below the spring, and by it were irrigated a dozen or more taro patches.” (Sterling and Summers)

Prehistorically and historically, the area of densest population in all the Hawaiian Islands was that flanking Waikīkī on the island of O‘ahu. Here the chiefs had their residences near the now famous beach and the offshore waters where conditions were ideal for their prized sport of surf riding.

A whaling captain, FD Bennett says that in Mānoa Valley yams were grown ‘chiefly for the supply of shipping.’ Menzies with Vancouver in 1792, described the plantations behind Waikīkī as ‘little fields planted with taro, yams, sweet potatoes, and the

cloth plant.’ (Handy, Handy & Pukui)

This in early times idyllic area was flanked by the great wet-taro lands of Mānoa, and the area between that valley and the sea which was one continuous spread of taro land and fishponds; by Pauoa, Nu‘uanu, Waiolani, Kapalama, and Kalihi. (Handy, Handy & Pukui)

Mānoa, due to its broad, well-watered valley, was probably settled early by the Hawaiians, who probably cleared much of the lower areas near streams for wetland taro cultivation.

“In upper Manoa the whole of the level land in the valley bottom was developed in broad taro flats . The terraces extended along Manoa Stream as far as there is a suitable land for irrigating.”

“Some of the lower portion of the old taro area, in land from the slightly elevated land south west of Rocky Hill, is now covered by streets and houses. But except for this, the extensive terrace area is still intact and could be replanted.”

“Most of it is under grass and unused. About 100 terraces are still being cultivated, but these do not constitute more than one tenth of the total area capable of being planted.”  (Sterling and Summers)

There was a famous terraced area below what is now the Punahou School campus. “Kauawaahila afterwards made some kalo patches [there], and people attracted by the water and consequent fertility of the place came and settled about ….”

“More and more kalo patches were excavated and the place became a thriving settlement. The spring became known as Ka Punahou, and gave its name to the surrounding place”. (Nakuina, Thrum 1892)

The first recorded landlord (Konohiki) of Kapunahou was Kame‘eiamoku, one of the twin supporters of Kamehameha I. This was in 1795.  The twins were originally Kamehameha’s guardians (Kahus) and later supported his rise to power.

In recognition of this support, Kamehameha gave Moanalua and Kapunahou to Kame‘eiamoku. Kameʻeiamoku died at Lahaina in 1802. Kapunahou passed on to his son, Ulumaheihei. Ulumaheihei was renamed Hoapili by Kamehameha I.

Hoapili lived at Kapunahou for, some twenty years and when Kamehameha I stayed at Waikīkī (1804-1811) he visited Hoapili there. Hoapili gave Kapunahou to his daughter, Liliha. This probably happened when Hoapili moved to Lahaina to become the Governor of Maui.

Liliha was married to Boki, the Governor of O‘ahu.  Shortly after this, Ka‘ahumanu, Queen Regent, became an ardent supporter of the missionaries who had arrived in 1820.

In 1829, she wished to give Hiram and Sybil Bingham a gift of land and consulted Hoapili. He suggested Kapunahou (although he had already given it to Liliha).

According to A. F. Judd, “Not unnaturally, Liliha demurred the proposal, but Boki consented. And Liliha’s resentment could avail nothing against the wish of her father, her husband, and the highest chief of the land.” The land was given to the Binghams, but by missionary rules, it was really given to the mission as a whole.

© 2025 Ho‘okuleana LLC

Filed Under: Buildings, Hawaiian Traditions, Schools Tagged With: Lily Pond, Hawaii, Punahou, Oahu College, Taro, Spring

July 20, 2024 by Peter T Young Leave a Comment

Ka Houpo o Kāne

E ui aku ana au ia oe,
Aia i hea ka Wai a Kane?
Aia i lalo, i ka honua, i ka Wai hu,
I ka wai kau a Kane me Kanaloa
He waipuna, he wai e inu,
He wai e mana, he wai e ola,
E ola no, ea!

One question I ask of you:
Where flows the water of Kane?
Deep in the ground, in the gushing spring,
In the ducts of Kane and Loa,
A well-spring of water, to quaff,
A water of magic power-
The water of Life!
Life! O give us this life!
(Emerson; Unwritten Literature of Hawaii)

Precipitation includes rain, snow, and fog drip. Evapotranspiration is the water that is either evaporated directly into the atmosphere or that which is used by plants and transpired back into the atmosphere. Runoff is the component that contributes to streamflow.

Groundwater recharge is the component of precipitation that percolates into the subsurface and is not lost to the atmosphere via evapotranspiration.  (Intera)

Fresh water travels down into the earth through a process called percolation. On the Hawaiian Islands, water first percolates through soil, if present, then through porous volcanic rock to the water table within the lava. (BWS)

During the volcanic eruptions that created the Hawaiian Islands, molten rock beneath the surface flowed up from the center of the volcanoes; dikes formed when magma stopped flowing to the surface, then cooled over time to form dense, nonporous rock.

Fresh water percolating down between the dikes compartment becomes trapped between the nearly impenetrable walls of the dikes. The water can only escape when its level rises and overflows the walls of the dike, or when great internal pressure causes leakage. Sometimes a freshwater spring will form above ground when such water spews from a dike. (BWS)

Sometimes percolating water becomes trapped when it meets layers of fine volcanic ash or clay-like soil that occur between the remnants of Hawaii’s ancient underground lava flows.  This perched water can no longer seep downward, so it collects and moves sideways, sometimes appearing as a spring (BWS)

“Ka-houpo-o-Kāne (literally, The-bosom-of Kāne), is the sacred region of Mauna Kea (between the 10,000 – 11,000 foot elevation), in which are found the springs fed by Ka-wai-hū-a-Kāne; by a rivulet from Waiau to the head of Pōhakuloa Gulch.” (“Houpokāne is mistakenly written Hopukani on most maps dated after 1900.”) (Maly)

Ka Houpo o Kāne represents the springs of the island of Hawaii. (Vredenburg)  “The area identified as Ka-houpo-o-Kāne is situated below Waiau, on the southwestern slopes of Mauna Kea, in the land of Ka‘ohe.”

“The god Kāne is believed to be foremost of the Hawaiian gods, and is credited with creation, procreation, light, waters of life, abundance, and many other attributes.”

“A land being likened to the chest of Kāne, can imply that the land was cherished and blessed by the god Kāne. … SN Hale‘ole’s tradition of Lā‘ie-i-ka-wai (In Kū ‘Oko‘a 1862-1863), records that “Kahoupokane” was one of three companions of Poli‘ahu. The other two companions were Lilinoe and Waiau.”

“The area identified as Ka-houpo-o-Kāne is situated below Waiau, on the southwestern slopes of Mauna Kea, in the land of Ka‘ohe.” (Maly)

“One of the primary attributes of Kāne are the wai ola (life giving waters), sacred springs and water sources made by Kāne around the islands, to provide for the welfare of the people and the land). Interestingly, at Kahoupo-o-Kāne are found the waters of Pōhakuloa, Hopukani, and Waihū (also known by the name “Ka-wai-hū-a-Kāne”).   (Maly)

“A spring on the southern side of the mountain, called ‘Wai Hu,’ is believed by the natives to be connected with [Lake Waiau].” (Pacific Commercial Advertiser, Sep 14, 1892)

“The few small springs on the glaciated peak of Mauna Kea in Hawaii are fed by ground water perched on and in glacial drift deposits. Their presence is note-worthy because of the light they throw on geologic history and on hydrologic principles rather than for the amount of water produced.”

“Springs in Hawaii fall into two chief categories: (1) high-level springs fed by ground-water bodies perched on or confined by intrusive bodies, ash beds, or modem or ancient soils and (2) basal springs fed from a great body of ground water which is kept in hydrostatic balance with sea water at a few feet above sea-level.” (Wentworth & Powers)

“Conditions on Mauna Kea favor rapid percolation of most rain and meltwater from the winter snow. Toward higher elevations rock-weathering becomes progressively more physical in type.”

“The largest springs on Mauna Kea are found at several points in the Waihu branch of Pohakuloa Valley, on the southwest slope between 8,900 and 10,400 feet.”

“The upper part of the Waihu springs area forms, in summer, a notably green little valley with many small patches of lush grass quite in contrast to the almost complete barrenness of the surrounding terrane, which is above timber line.”

“In the area to the east and up the slope from the springs are numerous small heaps of pre-European stone adz workings.  Certain lava caves contain evidence of habitation, suggesting that the springs were frequented by adz workers.”

“In addition to these larger springs there are some dozens of smaller seeps where trickling water or greener vegetation shows the emergence of small amounts of ground water.” (Wentworth & Powers)

© 2024 Ho‘okuleana LLC

Filed Under: Hawaiian Traditions, Economy Tagged With: Ka-wai-hu-a-Kane, Kahoupokane, Spring, Hawaii, Mauna Kea, Pohakuloa, Water, Houpo O Kane

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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.

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