The Hawaiian Archipelago - Six Months Among The Palm Groves, Coral Reefs, And Volcanoes Of The Sandwich Islands By Isabella L. Bird
















































































































 -   Its height is 760 feet, and its crater
nearly as deep, but its cone is rapidly diminishing.  Some years
ago - Page 134
The Hawaiian Archipelago - Six Months Among The Palm Groves, Coral Reefs, And Volcanoes Of The Sandwich Islands By Isabella L. Bird - Page 134 of 244 - First - Home

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Its Height Is 760 Feet, And Its Crater Nearly As Deep, But Its Cone Is Rapidly Diminishing.

Some years ago, when the enormous quantity of thirty-six inches of rain fell in one week, the degradation of both exterior and interior was something incredible, and the same process is being carried on slowly or rapidly at all times.

The Punchbowl, immediately behind Honolulu, is a crater of the same kind, but of yet more brilliant colouring: so red is it indeed, that one might suppose that its fires had but just died out. In 1786 an observer noted it as being composed of high peaks; but atmospheric influences have reduced it to the appearance of a single wasting tufa cone, similar to those which stud the northern slopes of Mauna Kea. There are a number of shore craters on the island, and six groups of tufa cones, but from the disintegration of the lava, and the great depth of the soil in many places, it is supposed that volcanic action ceased earlier than on Maui or Hawaii. The shores are mostly fringed with coral reefs, often half a mile in width, composed of cemented coral fragments, shells, sand, and a growing species of zoophyte. The ancient reefs are elevated thirty, forty, and even 100 feet in some places, forming barriers which have changed lagoons into solid ground. Honolulu was a bay or lagoon, protected from the sea by a coral reef a mile wide; but the elevation of this reef twenty-five feet has furnished a site for the capital, by converting the bay into a low but beautifully situated plain.

The mountainous range behind is a rocky wall with outlying ridges, valleys of great size cutting the mountain to its core on either side, until the culminating peaks of Waiolani and Konahuanui, 4000 feet above the sea, seem as if rent in twain to form the Nuuanu Valley. The windward side of this range is fertile, and is dotted over with rice and sugar plantations, but the leeward side has not a trace of the redundancy of the tropics, and this very barrenness gives a unique charm to the exotic beauty of Honolulu.

To me it is daily a fresh pleasure to stroll along the shady streets and revel among palms and bananas, to see clusters of the granadilla and night-blowing cereus mixed with the double blue pea, tumbling over walls and fences, while the vermilion flowers of the Erythrina umbrosa, like spikes of red coral, and the flaring magenta Bougainvillea (which is not a flower at all, but an audacious freak of terminal leaves) light up the shade, and the purple-leaved Dracaena which we grow in pots for dinner-table ornament, is as common as a weed.

Besides this hotel, and the handsome but exaggerated and inappropriate Government buildings not yet finished, there are few "imposing edifices" here. The tasteful but temporary English Cathedral, the Kaiwaiaho Church, diminished once to suit a dwindled population, but already too large again; the prison, a clean, roomy building, empty in the daytime, because the convicts are sent out to labour on roads and public works; the Queen's Hospital for Curables, for which Queen Emma and her husband became mendicants in Honolulu; the Court House, a staring, unshaded building; and the Iolani Palace, almost exhaust the category.

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