Mokuola

Mokuola, in Hawaiian culture, is a place of healing.  A rock just off its shore is believed to have healing powers, and people who were sick have come to Mokuola to swim around the rock in the hopes of healing their ailments.  (Miller)

People came here for spring water believed to have healing qualities; umbilical cords of infants were hidden here under a flat stone known as Papa-a-Hina (stratum of Hina) to protect them from rats.  (Pukui)

A sea pool to the right of the landing on the island was called Puaʻa-kāheka.  Just outside of Mokuola is a small islet called Kaulaʻi-nā-iwi, literally ‘dry the bones’ (bones of chiefs were dried here.)  (Hawaii County)

Occasional reference is made to Mokuola (also now called Coconut Island) as the place of refuge of the Hilo district, hence its name, life island. Careful enquiry shows that the area of this puʻuhonua included also a portion of the mainland adjoining. The heiau connected with it, named Makaoku.  (Thrum)

Makaoku is an ʻili in Waiākea.  In 1909, the Territory set aside 3.5-acres in the ʻili of Makaoku, Waiākea as the Kauikeaouli Park.  Today, the Liliʻuokalani Gardens (the Japanese Gardens) and associated land has a land area of about 30-acres and includes this former park named for the earlier king.

Mokuola was repeatedly struck when tsunami entered Hilo Bay.

“We have had a great disaster at Hilo … at 5 o’clock it swept in, in a mighty wave, washing up and into nearly all the stores … But at Waiākea the damage was frightful. … There has been nothing like this tidal wave since the year 1837 … when many grass houses were destroyed.”  (Severance, Pacific Commercial Advertiser, May 26, 1877)

“The water was 3 inches deep in Conway's store, when the 5 o'clock wave came In. The wave at Waiakea must have had a perpendicular height of 16 feet, to have taken the bridge and wharf where they now lie. The water swept completely over Cocoanut Inland, and the hospital there has disappeared.”  (Severance, Pacific Commercial Advertiser, May 26, 1877)

A tsunami struck again. “Cocoanut Island was pretty well wrecked. The wave swept it completely.  The old house formerly used by the keeper of the island, was turned completely around and swept seaward for a distance of about 20 feet and then laid flat on the ground.  A tall cocoanut tree, directly in its path was snapped off at the ground. The bathhouses were also torn down and moved some 12 feet nearer the landing place.”  (Hawai‘i Herald, February 8, 1923; Miller)

There is a coconut palm on the Island with small bands that indicate the maximum wave height of tsunami that washed over the island (8-feet, 1957; 12-feet, 1952; 15-feet, 1960; and 26-feet, 1946.)

The Spanish-American War was a conflict in 1898 between Spain and the United States, effectively the result of American intervention in the ongoing Cuban War of Independence.  Back then, Spain had interests in the Pacific, particularly in the Guam and Philippines.  Although the main issue was Cuban independence, the ten-week war was fought in both the Caribbean and the Pacific.

In the Islands, there was no assigned garrison here until August 15, 1898, when the 1st New York Volunteer Infantry regiment and the 3rd Battalion, 2nd US Volunteer Engineers landed in Honolulu for garrison duty.  They setup camp (‘Camp McKinley’) at Kapiʻolani Park.

Later (November 8, 1898,) approximately 200-soldiers of the 1st New York sailed from Honolulu to Hilo to inspect sites for a possible permanent military post – a highlight of their visit was a hike to the Kilauea volcano. The soldiers camped in the new wharf (just down the coast from Mokuola.)  (Greguras)

In 1900, the Hilo Swimming Club petitioned the government to designate Mokuola as a recreation area. Swimming facilities including a bathhouse and diving boards were built.

In 1910, a 30-foot-high wooden diving tower was built with platforms at 5-foot, 14-foot, and 30-foot levels. After it was destroyed in the tsunami of 1923, a stone tower was built with two levels, steps, springboards, and railings.

At the beginning of World War II, the military took control of Coconut Island, and the Navy used this tower to train troops in amphibious warfare.  (Valentine)

This was not the only military use on the Island.  In 1942, Mokuola USO was established, and recreational and training facilities were constructed there for American soldiers.  The facilities were officially opened to soldiers in 1943.  (Miller)

During the war, the island was restricted to military personnel. On two days per week, however, lady friends of servicemen were allowed to visit the USO, which was accessed by a pontoon bridge, the first bridge to the island. During the occupation, a new pavilion, showers and restrooms were built. The military gave the island back to the county in 1945. (Valentine)

When the island was finally turned over to the county in 1945, the pontoon bridge was put off-limits due to it being a “hazard to children and too costly to maintain.”

Boat service between the island and the shore resumed until April 1, 1946 when a devastating tsunami once again destroyed all of the structures on Mokuola except for a concrete diving tower that is believed to have been constructed by the Army Corps of Engineers for training purposes.  (Miller)

The 1960 tsunami washed completely over the island, destroying all buildings and the new bridge there. For three years, Mokuola was abandoned.

Funds were eventually allocated for a major restoration project of the island, including a new metal and concrete bridge, and new concrete walls to slow erosion.

By 1969 the bridge was completed and the park was re-opened to the public.  (Miller)  It remains a public park.

The image shows Mokuola. (DMY)   In addition, I have added others similar images in a folder of like name in the Photos section on my Facebook and Google+ pages.

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Kanakea Pond

In the Waiākea area called Keaukaha (‘passing current’) at Hilo on the Island of Hawaiʻi a legend refers to a hole called Kaluakoko beneath the water.

A man and a woman lived nearby, and later a second woman came to live with them.

The new wife became jealous of the first, and convinced her to go net fishing one day when the husband was fishing, though the husband had forbidden it because it would affect his fishing.

As she caught shrimp at the edge of a large hole, the second wife pushed her into the hole and covered the entrance with a rock, killing her. Blood spread through the sea foam and the fisherman, followed its trail in his canoe, moved the stone, and saw what had happened.

He confronted the second wife, who lied, and then beat her to death. According to the story, the hole has been referred to as Kaluakoko (‘the Hole of Blood.’) (Cultural Surveys)

Here, Kanakea (‘wide stream’) pond is located. A freshwater subterranean spring rises from a large sinkhole and feeds cold water into the bay at a former fishpond.

Due to apparent remnant of a seaward rock wall at the narrowest point of the channel to the ocean, it is believed to be a loko kuapā.  A cobble field, submerged except during low tide, is in a linear pattern, suggesting they may have been in the formation of the pond wall.  (However, the cobbles may have simple accumulated there by currents or tsunami.)

“There are plenty of ducks in the ponds and streams, at a short distance from the sea, and several large ponds or lakes literally swarm with fish, principally of the mullet kind.”

“The fish in these ponds belong to the king and chiefs, and are tabued from the common people. Along the stone walls which partly encircle these ponds, we saw a number of small huts, where the persons reside who have the care of the fish, and are obliged frequently to feed them with a small kind of muscle, which they procure in the sands round the bay.”  (Ellis, 1823)

“On the nights of high tides every keeper slept by the mākāhā of which he had charge. It was the custom to build small watch houses from which to guard the fish from being stolen at high tide, or from being killed by pigs and dogs; when the tides receded the fish would return to the middle of the pond, out of reach of thieves.”

“On these nights, the keeper would dip his foot into the water at the mākāhā and if the sea pressed in like a stream and felt warm, then he knew that the sluice would be full of fish.”  (Kamakau; Maly)

Railway tracks crossed the pond from about 1916 until 1946 (when they were destroyed by a tsunami;) remnants of the railroad trestle are still visible within and above the surface of the pond.  (Hawaiʻi County)

The pond’s modern name is ‘Ice Pond’ (due to the cold spring-fed waters.)  It is brackish (that word comes from the Middle Dutch root ‘brak’ (‘salty.’))

The adjoining small bay consists of white sand and coral rubble; between 1925 and 1930, coral material dredged from Hilo harbor was deposited on the western side.

The small bay is now referred to as ‘Reed’s Bay.’  It is named after William H Reed. Born in 1814 Belfast, Ireland, Reed was a businessman. He created Reed’s Landing, which he used to moor boats carrying lumber for one of his businesses.  (Hawaiʻi County)

Reed arrived in the Islands in the 1840s and set up a contracting concern specializing in the construction of wharfs, landings, bridges and roads.  Other interests included ranching, trading and retailing.  (Clark)

Across Hilo Bay, Reed also bought an island in 1861, originally known as ‘Koloiki’ (‘little crawling,’) once surrounded by the Wailuku River and Waikapu Stream.

Reed married Jane Stobie Shipman on July 8, 1868 (she was a widow, previously married to William Cornelius Shipman, a missionary assigned to Waiʻōhinu in the district of Kaʻū.  Shipman died in 1861, leaving Jane with her three children, William Herbert, Oliver Taylor and Margaret Clarissa.)

Jane was born in Scotland. At an early age she came to the US with her parents, lived in Quincy, Illinois, and was educated to be a teacher; and in 1853 was married to Reverend Shipman.  (The Friend, December, 1902)

Following his death, Jane moved to Hilo, with her three children and maintained the family by keeping a boarding school until 1868 (when she was married to Reed.)  (The Friend, December, 1902)

William Reed died on November 11, 1880 with no children of his own; Jane inherited the Reed land holdings.  (In 1881, Reed’s stepson William Herbert Shipman and two partners (Captain J. E. Eldarts and Samuel M Damon) purchased the entire ahupuaʻa of Keaʻau, about 70,000-acres from the King Lunalilo estate.)

The image shows the damaged rail line at Kanakea Pond.  (Hawaiʻi County)  In addition, I have included other related images in a folder of like name in the Photos section on my Facebook and Google+ pages.

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Hilo Bay and Breakwater

Legendary sources indicate that Hilo (‘to braid’) was, among other things, renowned for its rain and fertility.  Hilo is likely to have been one of the first Polynesian settlement areas on Hawai‘i Island; oral history and local legend indicate that Polynesians first settled Hilo Harbor around 1100 AD.

Early settlers would have found a protected bay, surrounded by fertile lands for agriculture, and well watered by regular rainfall and natural springs.  Natural waterways and wetlands were modified to create fishponds and planting areas.

Early accounts of Hilo Bay describe a long black sand beach stretching along present day Bay Front from the Wailuku River to the Wailoa River. Coconut Island is just east of the Wailoa River, and Reed’s Bay and Kūhiō Bay are just east of Coconut Island.

"The romantic might easily imagine Hilo to be a very inviting location ... on account of the beauty, grandeur, and wonders of nature, which are there so interesting. ... even by the sober, pious mind, to be now a desirable residence, because the wonders of nature and the wonders of grace are there united and so distinguished."  (Hiram Bingham)

Hilo was a Royal Center for many of the early chiefs.

When Captain George Vancouver arrived at Hilo Bay in 1794, Kamehameha was living at Waiākea and preparing his fleet of war canoes for his coming conquest of the other Hawaiian Islands, which ultimately led to the consolidation of the Hawaiian Kingdom.

Vancouver's crew surveyed Hilo as a potential anchorage, but found the surf too problematic to effect a landing and declared the bay only marginally sufficient for anchorage.

Missionary William Ellis arrived in Hilo Harbor in 1823, when the main settlement there was called Waiākea. Christian missionaries continued to come to Hilo Harbor until the mid-19th Century. The missionaries were followed by trade ships and whalers that used the Hilo Harbor port.

Hilo Bay is partially protected by a reef located in 10 to 20 feet of water (later named Blonde Reef after Lord Byron's vessel, HMS Blonde, which successfully anchored there in 1825.)  (The Blonde had carried the bodies of Liholiho (who was born in Hilo) and Kamāmalu back from London, where they died from measles during a visit there.)

Between 1824 and 1848 Hilo became a significant center for foreign activities, primarily as a result of the establishment of religious mission stations by American missionaries.

By 1874, Hilo ranked as the second largest population center in the islands, and within a few years shortly thereafter Hilo with its fertile uplands, plentiful water supply, and good port became a major center for sugarcane production and export.

Passengers and cargo landed at Hilo in the surf along the beach until about 1863, when a wharf was constructed at the base of present day Waiānuenue Street.

At one time both cargo and passengers were hoisted in a basket-like sling out to a waiting row boat which took the goods or passengers to the waiting ship. If the weather was rough, landing took place on the beach.

The wooden wharf was replaced by an iron pile wharf in 1865, and was extended between 1889 and 1890. Raw sugar was brought by inter-island steamships from the Hāmākua coast to Hilo before being shipped overseas.

The northern side of the bay became a focal point for the community's trade and commerce.  During this time, Hilo was ranked as the third most frequented port for whaling vessels in need of repair and re-provisioning.

With its foundations in the missionary Hilo Boarding School, commercial sugarcane cultivation and sugar production became the central economic focus for the Hilo area lasting until the 1970s.

The Waiākea Mill Company, in operation between 1879 and 1948, with thousands of acres of cultivated fields, established its mill operation at Wailoa Pond.

The Reciprocity Treaty (1876) between the Kingdom of Hawaiʻi and the US, along with the increase in commerce associated with the growing sugar industry and improvements in transportation in the Hilo area, prompted the decision that a harbor facility should be built on the calmer Waiākea side of Hilo Harbor. The government wharf at Waiākea was constructed at Kalauokukui Point between 1897 and 1899, and was upgraded in 1902.

Hilo Bay was still unprotected from high winds and storm surges that caused ships to break loose from their moorings and risk grounding.

In the late 19th century, the growing sugar industry in East Hawai'i demanded a better and more protected port, and a breakwater was constructed on Blonde Reef to shield ships from rough waters as they entered Hilo Harbor.

In 1908, construction began on a breakwater along the shallow reef, beginning at the shoreline east of Kūhīo Bay. The breakwater was completed in 1929 and extended roughly halfway across the bay. In 1912, contracts were awarded to construct Kūhiō Wharf, to dredge the approach to the new wharf, and to lay railroad track into the new harbor facility.

Work was completed at Kūhiō Wharf, Pier 1 in 1916. Pier 1 was a 1,400-foot long by 150-foot wide wharf with a wooden storage shed.  By 1917, a mechanical conveyor for bagged sugar with derricks for loading ships, was constructed.

In 1923, Pier 2 was constructed just west of Pier 1. Additional dredging was conducted in Kūhiō Bay as part of the construction. By 1927, Pier 3 was added on the west side of Pier 2.

Between 1927 and 1928, the approach to Pier 3 was dredged and the pier was widened.  In 1929, the 10,080-foot long rubble mound breakwater was completed.

Contrary to urban legend, the Hilo breakwater was built to dissipate general wave energy and reduce wave action in the protected bay, providing calm water within the bay and protection for mooring and operating in the bay; it was not built as a tsunami protection barrier for Hilo.

In fact, in 1946, Hilo was struck by a tsunami generated by an earthquake in the Aleutian Islands; it was struck again in 1960 by a tsunami generated by the great Chilean earthquake - both tsunami overtopped the breakwater and Hilo sustained significant damage, including to the breakwater.

(Lots of information here from Rechtman and Drennan.)  The image shows Hilo Bay and its breakwater (USACE.)  In addition, I have added other images to a folder of like name in the Photos section on my Facebook and Google+ pages.

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