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CONTENTS
Chapter 1: Sandwich Islands
True Name, Situation, Number and Extent Harbors General Appearance and
Structure Rain Windward Sides Leeward Sides Minerals Salt Lake
Soil Vegetable Productions Insects Animals Fishes Climate
Winds Storms Diseases Earthquakes Phenomena of Tides Meteoric Showers of 1825
Water
Spouts
Chapter 2: Early Hawaiian History Former intercourse between
the Hawaiian Islands and the Tahitian, Samoan and Marquesan groups
Superstition of "Youth-renewing Fountain" Creation of first inhabitants
Flood Origin of the World of Hawaii Traditions Ancient Hawaiian
Kings, Government, Common Law, Cruelties Kingly power Police Chiefs
Retinues Rank Orders of nobility Homage Public councils and
meetings Conduct of superiors towards inferiors Litigation Ordeals
Praying to Death Sorcery Soothsayers or Magicians Character of
Religion Notions of Future State Hawaiian Hades Ideas in regard to
souls Milu Idols Different classes of male and female God Lono
Goddess Pele and her family Hawaiian Centaur Fabrication of Idols
Temples or heiaus Ceremonies attending consecration Human sacrifices
Animal and vegetable offerings Diviners Priesthood Ranks General
character Taxes of priesthood Remarkable privileges Taboos Origin
and meaning of the word Present application Penalties attached to
violation of Cities of Refuge Comparison between the religions and
governments of the different groups
Chapter 3: Warlike weapons Armor Feather cloaks
and helmets War Preparation Militia Camps Mode of fighting
Victors and vanquished Truce Peace Festivals Orators and Bards
Songs Wailing Games Dances Mourning ceremonies Arts and
Agriculture Houses Ceremonies before occupying Clothing Food
Fisheries Commerce between different islands Stated fairs Method
of computation Knowledge and practice of medicine Origin and cure of
diseases Modes of burial Division of time Hawaiian dialect
Chapter 4:
Physical appearance
of the Hawaiians Chiefs Habits of Common people Women Marriage
Affinities of blood Friendships Salutation Cannibalism
Intemperance Treatment of sick Lunatics Aged Infanticide
Examples of Treatment of women Taboos of food General character of
the Hawaiians previous to contact with the whites
Chapter 5: Visits to the Hawaiian
Islands previous to Cook Anson's chart Spaniards acquainted
Shipwreck at Kealakeakua Bay Ships seen First appearance of Cook
His reception Astonishment of islanders Effects of visit War on
Maui Cook's re-appearance First notice of Kamehameha Cook's
arrival at Kealakeakua Bay His deification Remarks Native
hospitality Thefts Cook's desecration of the temple Growing
dislike of natives Ships sail Return Succeeding events Cook's
death Ledyard's account Native do Review of proceedings Recovery
of bones Peace Departure of ships Touch at Oahu Arrive at Kauai
Wars Attacked by natives Visit Niihau Final departure
Chapter 6: 1779 Unfavorable opinion entertained of the
islanders in consequence of the death of Cook Death of Kalaniopuu
War of succession Victories of Kamehameha Kamehameha conquers Maui,
Lanai and Molukai Arrival of Captains Portlock and Dixon Trade
opened Meare's visit Trade La Perouse visits Maui, 1786 Maui,
Lanai and Molokai rebel Arrival of the Eleanora Capture of boat and
murder of a sailor Metcali's bloody revenge Fair American captured
John Young and Isaac Davis made prisoners Difficulties between traders
and the islanders Kameharneha's indignation at the capture of the Fair
American Treatment of prisoners Kaiana's ambitious views Attempts
on vessels Vancouver's arrival First notice of Kanmualii Doedalus
arrives at Oahu Massacre of Lieutenant Hergest and Mr. Gooch Avarice
of chiefs Intercourse with Vancouver Kaahumanu Princely
hospitality Jealousy of other chiefs Cattle first introduced at
Hawaii Discipline of ships Orders of the king Widow of Kalaniopuu
Sham battle Present to King George III Transactions at Maui
Murderers executed at Oahu Festival of Makahiki Benevolent efforts
of Vancouver Theatrical entertainments Cession of Hawaii Departure
of Vancouver 1794
Chapter 7: 1794, Honolulu harbor discovered Murder of
Messrs. Brown and Gardner, January 1, 1795 Capture and recapture of
the Jackall and Prince Le Boo Troubles in Kauai Maui, Molokai and
Lanai subdued, 1794 Oahu invaded Kaiana's defection, rebellion and
death Visit of H. B. M. ship Providence, Captain Brougkton Marines
slain at Niihau Kamehamehas proposed conquest of Tahiti Completes
his conquests Kauai submits Humane policy of the conqueror
Government Courtly etiquette Laws Internal regulations Foreign
policy Trade Preparations for conquest of Kauai 1802 Great
tality Character of Kaumnalii His preparations Final settlement of
difficulties Arrival of Lisiansky 1804 Young, Governor of Hawaii
Attempt to convert Kamehameha Sydney Bay convicts Foreign settlers
Number Campbell Death of Davis, 1810 Kamehameha's wealth
Queens Liholilio, his heir Birth Character King returns to
Hawaii Public works Attempt of Russians in Kauai, 1814 Kotzebue,
1816 Birth Kamehameha's desire to hear of the Christian religion
Death, May 8th, 1819 Sacrifice of dog Native account of his funeral
obsequies
Chapter 8: 1819 Consequences of the death of Kamehameha
Scepticism Occasion of Abolition of idolatry National character Rebellion of Kekuokalani Defeat and death
1820 Arrival of American
missionaries Reception Hostile intrigues Kindness of Kaumualii Of
foreigners Tyranny and dissipation of Liholiho Gradual improvement of
Nation Voyage of Liholiho to Kauai, July, 1821 Kaumualii's hospitality Treachery of Liholiho Keeaumoku made governor of Kauai Kaahumanu's
marriage to Kaumualii and his son First Church erected at Honolulu Increased taxation January, 1822 First printing at the islands State of
education Arrival of English deputation Results Present of armed
schooner First Christian marriage Hoapili appointed governor of Maui New missionaries Increasing favor of government 1823 Festival in honor
of Kamehameha Illness and death of Keopuolani Foreign hostility to
missions Marriage of Hoapili Liholiho and train embark for England, 1824 Death of Kaumualii Rebellion at Kauai Final subjugation Last
heathen sacrifice performed by one of the royal family 1824 Conversion
of Kalaimoku and Kaahumanu Character of their administration News of
the death of the king Arrival of British Consul and family,
April, 1825
Chapter 9: Liholiho's passage to England Attention shown
to the party Death of King and Queen Boki's interview with George
IV Blonde frigate Arrival at Lahaina Honolulu Funeral Obsequies
Council of State Speeches Kaahumanu and Kalaimoku proclaimed
Regents Idolatry existing in Hawaii Courage of Kapiolani Singular
Creed Outrages of foreign Captains at Lahaina United States schooner
Dolphin at Honolulu, 1826 Triumph of the liberal party U. S. ship
Peacock Origin and structure of parties Character of English
Consul His policy Death of Kalaimoku, 1827 Laws enacted
Opposition of foreigners
Chapter 10: 1827 Arrival of Roman
Catholic Trusts Their history Reception Policy Opinion of chiefs
Foreigners Spread of Protestantism Boki's rebellion 1829 Conduct
of the King Legislation Hostility of foreigners Causes of Visit of
U. S. ship Vincennes Fatal expedition of Boki Persecution of
Papists Liliha's attempt at revolution Removal from office Kuakini
appointed Governor of Oahu Jesuits sent away Death of Kaahumanu,
1832 Succeeded by Kinau Kauikeouli assumes the government His
abolition of taboos Effects Reaction 1834
Chapter 11: 1836 Political position of the Chiefs and Mission
Mr. Richards' agency to the United States Employment of foreigners
Further history of the Jesuits Arrival of the French sloop-of-war Bonite
H. B. M. S. Alteon Lord Edward Russell Diplomatic intercourse Treaties
Return of priests from California, 1837 Ordered on board the Clementine
Abandoned to government Burning of the flag by English consul Armed
interference of Captains Belcher, of the Sulphur, and Du Petit Thouars,
of the Venus frigate Account of official intercourse Treaty negotiated
Arrival of Imogene frigate Another arrival of priests Sent away
Edict
against Romanism Further persecution Religious toleration proclaimed by
the king, 17th June, 1839 Proceeding of foreign residents at Honolulu
Admixture of religious and political movements of the French in the
Pacific Policy Arrival of L'Artemise frigate, Laplace commander Blockade
of the port of Honolulu Manifesto Demands Agreed to History of
commercial treaty Interview with king Arrival of French bishop Fresh
difficulties incited, 1842 Visit and demands of the corvette L'Embuscade,
Captaia Mallet, September
Chapter 12: Course of British Consul Appointment of Mr.
Richards to office 1838 Political state of the nation Constitution
1840 Code of Laws Temperance Societies Diplomacy of Charlton
Courts Sir
George Simpson Commissioners appointed to Europe 1842 Grant of lands
to Ladd & Co. Mr. Judd came into office Reform in Treasury Clandestine
departure of Charlton Letter to the King Alexander Simpson appointed
Consul and rejected Charlton dismissed Simpson's intrigues and violence
Suit of Pelly vs. Charlton Arrival of Lord George Paulet, February, 1843
Demands Cession of the Islands British Commission Troubles Withdrawal of
the King U. S S. Constellation Admiral Thomas Restoration of the Kingdom
Remarks upon the Cession
Chapter 13: Embassy to the United States
and Europe Acknowledgment of Independence at Washington Diplomacy in
London Paris Belgium Independence acknowledged by England,
and France Excitement in the United States A. Simpson
Correspondence between Mr. Fox and Mr. Upshur Claim of indemnification
on England Joint Guarantee of Great Britain and France "Times"
newspaper Return to the United States Death of Haalilio
HISTORY OF THE HAWAIIAN
ISLANDS
CHAPTER I
Sandwich Islands
True Name, Situation, Number and Extent Harbors General Appearance and
Structure Rain Windward Sides Leeward Sides Minerals Salt Lake
Soil Vegetable Productions Insects Animals Fishes Climate
Winds Storms Diseases Earthquakes Phenomena of Tides Meteoric Showers of 1825
Water
Spouts
That important cluster
of Islands, situated in the North Pacific Ocean, commonly known as the
Sandwich Islands, were so named by Captain Cook, at the date of their
discovery by him, in honor of his patron, the Earl of Sandwich, then
first Lord of the Admiralty.
Their legitimate
appellation, and the one by which they still continue to be
distinguished by the aboriginal inhabitants, is "Hawaii nei pae aina" a
collective term, synonymous with " these Hawaiian Islands. This term is
derived from the largest of the group, Hawaii, whence the reigning
family originated, and is gradually taking the place of the former.
The central situation
of the Hawaiian Islands in the vast North Pacific, is highly favorable
to their commercial growth. Their extremes of latitude are from 18° 50
to 22° 20 north, and of longitude from 154° 53' to 160° 15 west from
Greenwich.
This position is nearly
equidistant from Central America, Mexico, California, and the Northwest
Coast on the one side, and the Russian dominions, Japan, China, and the
Philippine Islands, on the other. When a civilized and enterprising
population shall have developed the resources of those countries, these
Islands will bear the same relative importance to them, in proportion to
their extent, that the West Indies now do to North and South America.
Including Bird Island, which was well known to the others prior to their
discovery, in 1778, the group consists of twelve.
The inhabited Islands,
eight in number, are of the following extent:
|
miles
long |
miles
broad |
square
miles |
Hawaii
Maui
Oahu
Kauai
Molokai
Lanai
Niihau
Kahoolawe |
88
48
46
22
40
17
20
11 |
73
30
25
25
7
9
7
8 |
4000
620
530
500
190
100
90
60 |
Bird Island is a barren rock, 129 miles to
the northwest of Kauai.
Three of the others are
equally unimportant; Molokini, an extinct crater of but slight
elevation, with one side open to the sea, lies midway between Maui and
Kahoolawe; Lehua, a mile to westward of Niihau, has an elevation of 1,000
feet, some slight vegetation, and an excellent spring of water; Kaula,
seven miles southwest from Niihau, is of less extent, and, like Bird
Island, abounds with wild fowl.
The whole embrace a
superficial area of about sixty-one hundred miles, of which Hawaii
includes two-thirds. But a small proportion of their coasts-, compared
with the Southern groups, is bounded by coral reefs. These are of
limited extent, and extend but a short distance from the shore, forming
a barrier, over which the sea rolls in sheets of foam.
There are few harbors,
though numerous channels occur in the reefs, affording entrance into
basins, capable of accommodating coasters. With the exception of
Honolulu, on the south side of Oahu, no really good harbour exists. At
Ewa, ten to the west of Honolulu, there is one with twelve feet at low
water on the bar. The basin within is sufficiently capacious to receive
the entire commerce of the Pacific; but the adjoining land is barren and
forbidding. At Koolau, on the north side of Oahu, there is another
harbor, with however but nine feet water in the channel. The surrounding
country is verdant, well watered, and the breeze directly from the
ocean. By deepening these channels, should the commerce of the kingdom
ever require it, fine sites for commercial towns would be formed.
Hilo Bay, on the north
of Hawaii, commonly known as Byron's Bay, affords excellent anchorage;
shipping are protected by a projecting reef, and the holding ground is
good, but the surf breaks heavily upon the beach, and not unfrequently
renders landing difficult. At all of the principal towns, with these
exceptions, the roadsteads are exposed; but such is the nature of the
prevailing winds, that vessels can frequent them in perfect safety
during nine or ten months of the year. With good ground tackle there is
little to be feared at any season. No dangers to navigation exist in the
vicinity of the Islands, with the exception of a reef off the west coast
of Kahoolawe. It is a little less than two miles from the shore, and
with two fathoms of water on it at low tide. A few rocks, within a
circumference of two hundred feet, comprise its whole extent.
The structure of the
group is volcanic. On Hawaii is found the largest known active volcano,
and several others of great size, partially or wholly quiescent. The
mountains attain an elevation of fourteen thousand feet. They are of
great extent and grandeur, and, throughout the group, present scenery of
peculiar and beautiful character. To the north they slope somewhat
precipitously to the sea, covered with a greensward at their base, and
above with dense forests. Plains are broken by deep ravines, down whose
steep sides cascades fall in bright and pretty sheets. Several; of these
often unite, as at Kauai, and form rivers of considerable depth and
size.
Palis, or precipices,
in many parts, present stupendous walls of rock, from one thousand to
three thousand feet perpendicular elevation, directly fronting the sea,
the surging of which forms large caverns into which the sea rushes with
stunning effect. To the windward, and on the highlands, there is
abundance of rain, which keeps vegetation perennially verdant. The
leeward portions, during most of the year, suffer from drought, and
offer a cheerless aspect. Below the region of clouds, vast and rugged
masses of broken lava spread themselves over the country.
Plains frequently occur
with a soil formed of ashes and cinders, which, easily set in motion by
violent gusts of wind, sweep over the land, and are carried to sea in
dense clouds. During the winter months, when the trades are partially
interrupted, showers often occur. When much rain falls the plains become
covered with a species of coarse grass, which affords tolerable
pasturage for cattle.
Extinct volcanoes are
very common. They are of every age, size and shape; at places, crowning
the summits of lofty hills and mountains; elsewhere rising precipitously
from plains or projecting into the ocean, they form prominent landmarks
for navigators. One of the most singular and well-known, is the
promontory near Honolulu, called Leahi, better known as Diamond Head,
from an idea once current that precious stones were to be found there.
The minerals are few
and simple, consisting of the usual variety of the lavas, from the most
solid and granular to the light pumice-stone. Ledges of compact
lime-stone, a good material for building, are found on several of the
Islands. These being elevated considerably above the sea, have caused
much speculation as to how they were formed or arrived at their present
situation. The most remarkable is at Kahuku, Oahu. No metals have been
discovered. Four miles to the west of Honolulu, and within a mile of the
ocean, is the famous salt lake of Alia-paakai, elevated only a few feet
above the level of the sea. It is in the "heart of a crater, nearly oval
in form, and about a mile in circumference. At certain seasons salt
forms spontaneously and in the greatest abundance; at others but little
is created, from its being overflowed by rains. Some have supposed it a
mineral salt; but the general belief among the natives is, that it is
formed by evaporation. The following facts favor the supposition. Its
general depth is but eighteen inches; near the centre* a hole exists,
five to six fathoms in circumference, which, as no bottom has been found
to it, is supposed to connect with the ocean. Through this the lake is
slightly affected by the tides, and at times it is crusted over with a
stratum of salt sufficiently strong to- bear a man's weight.
The soil of the Islands
is formed of decomposed volcanic rocks, sand, mud and ashes. To be made
fertile it requires constant irrigation. Valleys which receive the
debris and rains of the mountains, and for ages have been accumulating
deposits of vegetable mould, are exceedingly rich and productive; but
they are of limited extent. The soil generally is poor, better adapted
for grazing than cultivation, though with labor and skill it can be made
to produce good crops. Nature yields but little spontaneously and the
inhabitants have always been obliged to exercise much industry and
ingenuity in their farms.
The principle article
of food is the well known kalo (arum esculentum). Great labor is
necessary in raising it successfully and it requires a year or more to
arrive at maturity.
The banana, yam, sweet
potato, breadfruit, cocoanut, arrowroot, sugar-cane, strawberry,
raspberry, ohelo, (a berry,) ohia, (a juicy, red apple, but of poor
flavor,) are indigenous and plentiful. Many varieties of esculent fruits
and vegetables have been successfully introduced, among which are
melons, the delicious chirimoya from Peru, limes, oranges, guavas,
pine-apples, grapes, peaches, figs, citrons, and tamarinds.
The vegetables of the
temperate region have been acclimated to a considerable extent. The
uplands of Maui produce excellent "Irish potatoes." Wheat of good
quality thrives in the same region. An oil used in painting is extracted
from the nut of the kukui tree (aleurites triloba). Sandal wood,
suitable for exportation, is mostly exhausted, though the young wood is
abundant.
Coffee, cotton, indigo,
tobacco, sugarcane, mulberry, cocoa and most of the tropical plants can
be successfully cultivated on the low grounds, while the uplands are
suitable for the productions of more temperate regions.
Insects are few, though
there are some of a destructive character. A species of caterpillar, the
pelua, at certain seasons destroys vegetation to a great extent, eating
even the grass to its very roots. A slug deposits its eggs in the cotton
blossoms, which, when ripe, are pierced through by the young insects,
and the staple entirely destroyed. Large spiders are very numerous and
mischievous, weaving strong webs upon shrubs and young trees, in such
quantities as to greatly injure them. A species of woodlouse, the
ant-cow, is very annoying.
A sooty crust, firm,
hard and stiff, like strong paper, forms upon many varieties of trees
and plants, covering the bark and even the leaves, giving them the
singular appearance of being clothed in mourning. Rats destroy the
sugarcane to a considerable extent annually. Though the Hawaiian
agriculturist escapes many of the evils incidental to other tropical
climes, enough exist here to make his labors no sinecure. Noxious
vermin, such as mosquitoes, fleas, cockroaches, scorpions and
centipedes, are a modern importation and have extensively increased,
Serpents, frogs or toads have not as yet reached the Islands. A small
lizard is abundant.
The forests are usually
very dense, broken by deep chasms, hidden ravines and deep
conical-shaped pits, which appear to have once been active craters. The
trees are overgrown with masses of ferns and parasitical vines, thickly
interlaced and spreading their shoots in all directions, which render it
a task of great difficulty to penetrate their recesses. There are but
few birds to enliven these sylvan solitudes. Wild geese are found at
Hawaii; snipe, plover and wild ducks on all the Islands. A variety of
the owl is very common; but nature, inthe ornithological as well as the
entomological tribe, has been chary of her gifts, and the traveler looks
in vain for the endless varieties which the more favored intertropical
countries afford. Dogs, swine, rats and domestic fowls are indigenous,
and, beside the wild-fowl above mentioned, were the only varieties of
animal food before the introduction of cattle.
Fish, of which there
are a great variety, form one of the chief articles of diet. They
consist chiefly of the albicore, bonita, flying-fish, shark, eel, and
many species preserved in artificial ponds, which acquire a delicious
flavor, and are highly prized. The best of these is the mullet. Edible
shell-fish are also abundant, of which the pearl oyster, cuttle fish and
prawn are the most palatable. Pearls are common, but of no great size or
beauty. They formerly constituted a profitable branch of trade, and were
monopolized by the king. The common oyster is not found.
The climate is
salubrious, and possesses such remarkable evenness of temperature that
the language has no word to express the general idea of weather. The
tropical heat is mitigated by the trades, which blow over a wide expanse
of ocean in the temperate zone. The shores on either side show but
little difference in the results of the thermometer. Physiologists give
a certain point of temperature as most conducive to health and
longevity. The mean heat of these Islands approaches near to it, and is
highly favorable to the full development .and perfection of animal
economy.
By visiting the
interior and ascending the mountains any desirable degree of temperature
can be attained. On the highest mountains snow remains during much of
the year, and in exposed situations on Mauna Kea throughout the whole.
Snow storms occur on the highlands of Maui during the winter months.
On the upland region of
Kauai, a uniform elevation of four thousand feet, both snow and hail
occasionally occur. The temperature here is quite regular the year
through, requiring warm garments and fires even in the month of July.
The district is cold and wet, and of little value. A portion of it
supports a heavy growth of timber and is frequented only by
wood-cutters. The average temperature of Waimea, Hawaii, situated in the
interior, at an elevation of about four thousand feet, is nearly 64°
Fahrenheit 48° being the lowest extreme.
This place affords an
excellent retreat for those whose constitutions have become enervated by
too long a residence nearer the coast. Rains are frequent at this
altitude, but the dryness of the soil seldom leaves the ground damp for
any length of time. At Mountain Retreat, back of Lahaina, Maui, an
elevation of three thousand feet, the temperature varies from 40° to
75°; but such situations afford few comforts for the sick and their
dampness renders them otherwise objectionable.
Localities can be
selected on the seashore which possess advantages for invalids,
particularly those affected with pulmonary complaints. Many individuals
by change of residence, have prolonged their lives for years, and others
who in the less favored regions of the north were perpetual sufferers,
live with scarcely an admonition of their disease. Lahaina, Kailua, Ewa
and Honolulu have all a good reputation in this respect.
At the former, during
ten years, the highest thermo-metrical elevation was 86°; the lowest 54°;
an extreme difference of but 32°. During no day in this period was the
range greater than 19°. June has the highest range January the lowest.
But little rain falls and for successive months the sun is rarely
obscured by clouds.
The common range of the
thermometer at Honolulu is 12° per diem. The greatest degree of heat
during twelve years in the shade was 90°, and 54° for the coldest; the
mean about 75°. Kailua and Ewa vary but little from the above. At Koloa,
Kauai, the thermometer varies from 50° to 88°; at Waioli, from 55° to
90°, with much rain. A change of wind affects the climate materially.
During nine months of the year the northeast trade blows with great
regularity and the temperature is very uniform.
Oahu and Kauai are the
most influenced by it; Maui, which is larger, has in a few places to the
leeward, including Lahaina, the regular land and sea breeze. Hawaii,
from its size and height of mountains, neutralizes its influence, and
enjoys an almost uninterrupted land and sea breeze. This occurs, in some
degree, even on its northeast coast where the trade is usually freshest.
The winds partake of the character of the sea breeze in the day, and
during the night are so modified by the influence of the land, as to
vary their course from off the shore, or become very light.
Where the mountain
ranges are broken by steep defiles, as at Kawaihae and other bays on the
west side, the wind rushes through with great violence, gathering
strength as it descends until it passes off to sea in furious gusts.
During the winter months the trades are interrupted, winds from the
south and west often prevailing for several successive weeks; calms are
also frequent and of long duration. The south wind brings rain and is
usually loaded with a briny vapor injurious to vegetation. Its effects
are equally unpleasant to the human system. Headaches, catarrhs,
rheumatism, and kindred diseases, prevail during its continuance.
Upon foreigners its
influence is very obvious, causing a compression about the head and an
enervation which indisposes to mental or physical exertion; the
atmosphere becomes oppressive and at times feels like the heated air of
a furnace. The miasma arising from the lagoons to the southeast of
Honolulu is blown back upon the land, infecting the town with an odor
which but for its rarity would be insupportable. The natives call it the
'sick wind,' and with propriety. It sometimes occurs with sufficient
force to destroy their frail habitations and do much damage to
plantations and forests. Much of the weather at this season is however
of the most delightful description; the sky becomes cloudless, the
atmosphere dry, clear and bracing, and the whole system feels the
invigorating influence of the change. Nothing can exceed the
soft brilliancy of the moonlight nights. Thunder-storms are rare and
light in their nature. No hurricanes have been known.
Epidemic diseases are
few and of a light character. The mumps have prevailed very generally,
and in some cases terminated fatally through mismanagement. The
influenza occurs almost annually but is not often fatal unless added to
other causes. The whooping-cough, a few years since, spread through the
whole population, but soon entirely spent itself. Contagious diseases
are scarcely known, excepting those of a cutaneous nature, which very
generally prevail, owing to filthy habits and gross food. The small-pox
has raged in the southern groups, but has never reached here.
Vaccination is very generally practiced. The croup sometimes occurs.
Hoapiliwahine, a chief woman of high rank, upwards of seventy years of
age, died of this disease in January, 1842. Powerful volcanic eruptions,
attended with disastrous effects, have occurred on Hawaii several times
within the memory of the present generation. Some of the largest of the
craters, such as those of Mauna Haleakala, (house of the sun,) on Maui,
at an elevation of eleven thousand feet, have been quiescent from a
period beyond the traditions of the inhabitants.
Earthquakes are chiefly
confined to the largest island; the shocks felt at Maui are slight. The
immense craters with which the former island abounds operate as
safety-valves, by which the pent gases, generated by the vast
subterranean fires, escape. Without them, the thin crusts of lava which
constitute the foundation of the island, would be rent asunder, and it
would become a terrific waste. Shocks are indeed frequent, but without
sufficient strength to be very destructive. Trees are thrown down, rocks
split, and the scene of action otherwise affected. At Hilo, in November,
1838, during the space of eight days, from forty to fifty shocks
occurred.
Twelve distinct ones
were counted in one night. For two days and nights the earth was in a
state of continual agitation; the plants and flowers trembling like
frightened animals. In some cases the motion was perpendicular, like
that of a ship pitching, and attended by noises and sensations similar
to those produced by heavy waves striking against her sides, and some
degree of nausea was felt.
In others the action
was lateral, easy and undulating, unaccompanied by any sounds. In April
1841, several more powerful shocks were experienced at the same place,
one of which was quite severe. The houses were violently shaken, and had
they not been constructed of yielding materials, would have been
prostrated. The plastering was shattered, crockery-ware destroyed, milk
thrown from pans, stone walls cast down, and other damage done. In March
of the same year, several of a severe nature occurred at Kailua, which
threw down much rock from the pali. These shocks were distinctly felt
throughout Maui. On the 25th of September, 1825, a shower of meteoric
stones occurred at Honolulu.
Reports like the firing
of cannon and the repeated discharges of musketry were heard at about
ten o'clock in the morning. At first the supposition was that a naval
action was taking place in the immediate neighborhood; but the fall of
many fragments of rock, weighing from ten to twenty pounds, accompanied
by a whizzing sound, explained the nature of the noises. They struck
with sufficient force to create cavities in the coral rock, and the
pieces presented a grayish black exterior, with a yellowish appearance
on the fractured portions. A remarkable oscillation of the ocean was
observed in 1837 throughout the group. In 1819, one on a lesser scale
and unattended with any fatal consequences occurred. It was considered
by the natives as prognosticating some dire event to their nation, and
the death of Kamehameha, which took place soon after, was supposed to be
the consummation. Upon its recurrence in 1837, the death of his son
Kauikeouli or some high chief was confidently predicted; but as no
national calamity ensued, this superstition was materially weakened.
On the evening of the
7th of November, the commotion of the waters was first noticed at
Honolulu. Neither the barometer nor thermometer indicated any unusual
atmospherical changes. At five o'clock it was observed the sea was
retiring. This it did with such rapidity as to cause much alarm among
the foreigners, who were fearful its reaction would overwhelm the town,
like the great wave which destroyed Callao in 1746; but hundreds of the
native population, thoughtlessly shouting and frolicking, followed its
retreat, picking up the stranded fish, and viewing the whole as a rare
piece of fun. Some, however, seemed otherwise affected, and the dismal
wail which was raised in the stillness of the evening, earned the news
far inland.
The first recession was
the greatest, being more than eight feet; the reefs were left entirely
dry, and the fishes died. The vessels, not in the deepest water,
grounded; but the sea quickly returned, and in twenty-eight minutes
reached the ordinary height of the highest tides: it then commenced
receding again and fell six feet. It rose a few inches higher on its
third return and fell six and a half feet. This action continued, with a
gradually diminishing force and extent, throughout that night and the
forenoon of the ensuing day. The greatest rapidity with which it fell
was twelve inches in thirty seconds.
On Hawaii and Maui the
phenomenon was more powerful and occasioned considerable loss of
property and lives. Its action increased to the windward, the northern
sides of the islands being the most affected. At Maui the sea retired
about twenty fathoms and returned with great speed in one immense wave,
sweeping before it houses, trees, canoes and human beings. At Kahului
the inhabitants, as at Honolulu, followed with rapturous delight the
retreating wave, when suddenly it turned upon them, and rising like a
steep wall, rushed forward to the shore, burying the natives in its foam
and destroying the whole hamlet. The amphibious character of the
islanders proved their safety, though they were obliged to mourn the
loss of two of their number and the destruction of all their personal
effects.
At Byron's Bay, Hawaii,
the village was crowded with people, who had collected to attend a
religious meeting. At half-past six o'clock the sea retired at the rate
of five miles an hour, leaving a great portion of the harbor dry, and
reducing the soundings in other places from five to three and a half
fathoms. The wondering multitude, in their simplicity, eagerly rushed to
the beach to witness the novel sight; quickly a gigantic wave came
roaring towards them at a speed of seven to eight miles an hour, and
rising twenty feet above high-water mark, dashed upon the coast with a
stunning noise like a heavy crash of thunder. The people were buried in
its flood; houses, canoes, fish-ponds, animals, in short, property of
all kinds, were mingled in one common ruin. Cries of distress filled the
air. Those in the water were struggling for their lives amid the wreck
of houses or entangled among floating timber, while their relatives who
had escaped the torrent, were loudly bewailing their situation. The wave
which had rushed inland had in its way dashed over the deck of an
English whaler at anchor in the bay.
As soon as the crew
recovered from the shock, they lowered their boats and through their
exertions many lives were saved. Not a canoe had escaped, and numbers of
the people, stunned and insensible, were floating seaward. The
destruction of property was universal; even the garnered food was swept
off. In two hamlets alone, sixty-six habitations were destroyed and
eleven lives lost. Other portions of the sea-coast suffered in like
proportion. No shocks of earthquakes or any tremor of the earth were
experienced, though the action of the crater of Kilauea, the night
previous, was uncommonly furious. In some spots its fires were quenched;
in others, chasms were opened with violent explosions. It would appear
from the simultaneousness of the commotion throughout the group, that it
originated at some distance. The wave struck the several islands from
apparently the same direction.
May 17th, 1841, the
same scene, though on a much less violent scale, and attended with no
loss of life, recurred. At twenty minutes past five o'clock, P.M., the
water in the harbor of Honolulu was observed to be suddenly discolored
and breaking like a tide rip. It then rushed rapidly out, leaving a
portion of the harbor and all the reef bare. This occurred twice in the
space of forty minutes, when it resumed its ordinary appearance. The
fall was estimated at three feet. Simultaneously, at Lahaina, a distance
of one hundred miles, the rise and fall of the water was several feet,
and occurred frequently, at intervals of four minutes each, rushing
violently and with great noise over the reefs.
At about this period a
similar scene was noticed on the coast of Kamschatka.
An immense
water-spout broke over the harbor of Honolulu in May, 1809. The
atmosphere was clear and the day calm when it was first observed. A
heavy, dark cloud hung over its body, which appeared to be of the size
of a stout mast. As it advanced, its bulk increased, until it attained
the thickness of a hogshead. Its progress was slow, accompanied with a
violent ebullition of the water at its base. Upon touching the reefs,
the column broke, causing a sudden rise of the sea of three feet on the
beach. Great numbers of fish were destroyed by the weight of the mass of
water which fell. A few years before, one broke on the north side of the
island, washed away a number of houses, and drowned several of the
inhabitants. |
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