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August 16, 2024 by Peter T Young Leave a Comment

Hot Spot

Kupuna means elder, grandparent or ancestor. The islands to the northwest of the main Hawaiian Islands have been referred to as the Kupuna Islands. The Hawaiian chain is made up of volcanic islands.

Kilauea Volcano has been erupting since 1983. Mauna Loa is also an active volcano. Off the coast, to the southeast, Kamaʻehuakanaloa Seamount (previously known as Loʻihi) is forming. (It is currently about 3,000-feet below sea level and is estimated to emerge above sea level in the next 10,000 to 100,000 years.)

Some of the other recent eruptions include Hualālai that last erupted in 1801; Haleakala that last erupted in about 1790 and Mauna Kea that last erupted about 4,000 years ago. (SOEST) (The first three volcanoes are considered ‘active’ and the latter three ‘dormant.’)

Hawaiʻi sits over a ‘hot spot,’ the Hawaiian hot spot.

It’s one hot spot, but lots of volcanoes have formed over it. The Islands are above a moving sea floor of the North Pacific Ocean (the Pacific Ocean is mostly floored by a single tectonic plate known as the “Pacific Plate.”)

The Pacific Plate is moving over the layer in the Earth known as the Asthenosphere. This movement takes it to the northwest. As the plate moves over a fixed spot deeper in the Earth where magma (molten lava) forms, a new volcano can punch through this plate and create an island.

As the plate moves away, the volcano stops erupting and a new one is formed in its place. With time, the volcanoes keep drifting westward and getting older relative to the one active volcano that is over the hot spot.

As they age, the crust that they sit on cools and subsides. This, combined with erosion of the islands, once active volcanism stops, leads to a shrinking of the islands with age and their eventual submergence below the ocean surface.

Each island is made up of at least one primary volcano, although many islands are composites of more than one. The Big Island, for instance, is constructed of 5 major volcanoes: Kilauea, Mauna Loa, Mauna Kea, Hualālai and Kohala (the island is still growing, but is basically about 400,000-years old.)

Maui is made up of two volcanoes, Haleʻākala and West Maui (about 1.32-million years ago.) Kahoʻolawe and Lānaʻi were each formed by a single volcano of their respective names.

Molokai was formed by East and West Molokai volcanoes (about 1.8-million years ago.) Oʻahu is also formed by two, Koʻolau and Waianae (about 3-million years ago.) Kauai and Niʻihau were formed by volcanoes of their respective Island names (about 5.1-million years ago.)

They are all part of the Hawaiian-Emperor Volcanic Chain. About 40-million years ago, the Pacific Plate changed direction from north to northwest – so the Emperor Seamounts run more north-south, the Hawaiian Ridge north-westerly.

Midway Island is 27.7-million years old; Meiji Seamount the northern part of the Emperor Seamount (near the end of the Aleutian chain) is about 80-million years old.

All of these are still youngsters, when you look at the perspective, say, of the dinosaurs. The Islands weren’t even a glimmer in anyone’s eyes when dinosaurs walked the Earth; sixty-five million years ago the last of the non-avian dinosaurs went extinct, after living on Earth for about 165-million years. (USGS)

If all of Earth time from the very beginning of the dinosaurs to today were compressed into 365 days (1 calendar year), the dinosaurs appeared January 1 and became extinct the third week of September.

Using this same time scale, the Earth would have formed approximately 18.5-years earlier. By comparison, people have been on earth only since December 31 (New Year’s eve.) (USGS)

When I was at DLNR, President George W Bush created the Northwestern Hawaiian Islands Marine National Monument on June 15, 2006. Seeking a more appropriate Hawaiian name for the monument, suggestions for a name change were submitted.

We selected the name Papahanaumokuakea; it was submitted by Pua Kanahele. Pua and the First Lady, Laura Bush, attended the ceremony announcing the new name (March 2, 2007.)

The Kumulipo, the creation chant, tells of the history of how all life forms came and evolved from Papahanaumokuakea, beginning with the coral polyp – the building block for all life.

Papahanaumoku is a mother figure personified by the earth and Wakea is a father figure personified in the expansive sky; the two are honored and highly recognized ancestors of Native Hawaiian people.

Their union resulted in the creation, or birthing, of the entire Hawaiian archipelago. The naming of the monument is to honor and preserve these names, to strengthen Hawaii’s cultural foundation and to ground Hawaiians to an important part of their history.

Thus, the genealogy of Papahanaumokuakea tells the story of Native Hawaiians’ ancestral connection with the gods who created those coral polyps, the Northwestern Hawaiian Islands or Kūpuna Islands, and everything else in the archipelago. (Lots of information here from the UH-Manoa SOEST, USGS and Papahanaumokuakea.)

© 2024 Hoʻokuleana LLC

Hawaiian Ridge - Emperor Seamounts
Hawaiian Ridge – Emperor Seamounts
NWHI_Map-noting Kure
NWHI_Map-noting Kure
Loihi-compared to Hawaii Island
Loihi-compared to Hawaii Island
Papahanaumokuakea-Marine-National-Monument-Map
Papahanaumokuakea-Marine-National-Monument-Map
hawaiimap-loihi-SOEST
hawaiimap-loihi-SOEST
Hawaiian Islands - Emperor Seamounts
Hawaiian Islands – Emperor Seamounts
Hawaiian Archipelago
Hawaiian Archipelago
Age of Islands-map
Age of Islands-map
Hawaiian- Emperor Seamounts
Hawaiian- Emperor Seamounts
3D of Kamaʻehuakanaloa (Lo'ihi)
3D of Kamaʻehuakanaloa (Lo’ihi)
Papahanaumokuakea Naming Ceremony-postcard-signed by Pua Kanahele-03-02-2007
Papahanaumokuakea Naming Ceremony-postcard-signed by Pua Kanahele-03-02-2007
TectonicPlates
TectonicPlates
Plates
Plates
Hawaiian Islands for space-NASA
Hawaiian Islands for space-NASA

Filed Under: Place Names Tagged With: Hawaii, Papahanaumokuakea Marine National Monument, Hot Spot, Loihi, Kamaehuakanaloa

January 21, 2017 by Peter T Young Leave a Comment

Old-Young – Wet-Dry – East-West

“Agriculture was a matter of great importance in Hawai‘i, because by it a man obtained the means of supporting himself and his wife, his children, friends and domestic animals. It was associated, however, with the worship of idols.” (Malo)

“In the Hawaiian Islands agriculture was conducted differently on lands where there were streams of water and on dry lands. On lands supplied with running water agriculture was easy and could be carried on at all times …”

“… and the only reason for a scarcity of food among the people on such lands was idleness. Sometimes, however, the water-supply failed; but the drought did not last long.” (Malo)

All Polynesian societies descend from an ancestral culture which had first settled the western archipelagoes of Samoa and Tonga by about 1200 BC. Throughout this varied region, root-crop horticulture was transferred and adapted to local environmental conditions and challenges. (Kirch)

Most Polynesian archipelagoes have a volcanic ‘hot spot’ origin and, due to tectonic plate movement, islands increase in age as one progresses further from the hot spot of volcanic activity. The Hawaiian Islands illustrate this geological age progression, and associated opportunities for crop production.

The geographically older westerly islands (Kauai, O‘ahu, Molokai and west Maui) are more heavily weathered, with permanent stream flow and alluvium valleys, on which irrigation could be developed.

The agricultural emphasis was on taro irrigation, with shifting cultivation and other forms of dryland gardening providing a secondary role.

In the geologically younger islands to the east (east Maui and Hawai‘i), irrigation was only a minor contributor to subsistence production and highly labor-intensive, short-fallow dryland field systems predominated.

Most of the arable terrain is volcanically younger, lacking stream flow and prohibited the development of extensive irrigation works. Thus, irrigation systems in east Maui and Hawai‘i, while present in restricted areas, contributed in only minor.

Initial settlement was confined for the most part to the windward valley regions, with their more favorable ecological conditions (ample stream flow, higher rainfall, extensive alluvial soils.)

Later, there was a major expansion into leeward regions throughout the archipelago. The initial stages of this expansion focused on leeward valleys or around bays with rich marine resources.

By about AD 1400, settlements were moving into increasingly marginal environments, including the interiors of leeward valleys and the higher elevation slopes of the easterly islands.

It was a period of tremendous significance in Hawaiian history; during this time, (1) the population underwent a geometric rate of increase; (2) virtually all habitable and arable lands were occupied and territorially claimed; and (3) the territorial pattern of chiefdom (moku) and sub-chiefdom units (ahupua‘a) appears to have been established.

In addition, toward the end of this period the Hawaiian sociopolitical system was transformed from a simple, ancestral Polynesian chiefdom to a highly stratified society with virtual class differentiation between ali‘i (chiefs) and maka‘āinana (commoners.)

There were other differences in the political and religious structure of the eastern and western chiefdoms. In particular, the elaborate makahiki, or wet-season harvest ritual, as well as the emphasis accorded the cult of the war god Kū with its associated luakini temple ritual, was especially developed on Hawai‘i and Maui, less so on the westerly islands of O‘ahu and Kauai.

Of the four great Hawaiian gods (Lono, Kāne, Kanaloa and Kū,) Lono and Kane were both associated with agriculture, each showing different symbolic linkages, the one centered on Lono involving rainfall, sweet potato (and to a lesser extent dryland taro) and dryland cultivation, the other centered on Kāne involving flowing waters, taro and irrigation.

Lono was specifically the god of dryland cultivation and associated with “clouds bearing rain,” thunder, the sweet potato (the primary dryland crop,) the rise of Pleiades and the rainy season.

Kāne who was associated with pondfield irrigation of taro, running water (wai,) springs, fishponds, male procreative powers and irrigation. As noted by Handy & Pukui, “the family bowl of poi (starch staple made from taro) in the household was sacred to Haloa, who is Kāne, an ancestor in the line senior to man”.

“The control of agricultural production was one of the sources of power for the leasers if Hawaiian societies, societies which were among the most highly stratified in Polynesia at the time of European exploration.” (Tuggle)

The political formations and moves for territorial expansion just before ‘contact,’ show a pattern that corresponds closely to the fundamental differences in agricultural base. The aggressive, expansionist, Ku-cult centered chieftainships of Maui and Hawai‘i were precisely those polities most dependent upon intensified dryland field cultivation.

The frequent objects of their aggression were the western islands of Molokai, O‘ahu and Kauai, and their resource-rich centers of irrigation agriculture and fishpond aquaculture.

In these western islands, the possibilities for greater agricultural intensification remained substantial, despite high levels of population density, owing to the environmental conditions favoring irrigation.

The complex linkages between varied agricultural landscapes and the social relations of production – effectively, the ecological and cultural contrasts between ‘the wet and the dry’ – illustrate the role intensification played in the political evolution of chiefdom societies.

(The inspiration and information here is from Patrick Kirch’s book “The Wet and the Dry.” Maps are Natalie Kurashima’s Traditional Agriculture Maps.)

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Filed Under: Hawaiian Traditions, Economy, General Tagged With: Hot Spot, Hawaii, Loi, Kalo, Taro, Sweet Potato, Field System, Uala, Agriculture

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