FLORES TOURIST ATTRACTION, FLORES ISLAND - INDONESIA

LABUANBAJO

Labuhanbajo - West Flores - Indonesia

A little town inhabited by fishermen, lies at the extreme western part of Flores Island. The town serves as a jumping off point for the trip to Komodo Island. It is a beautiful area for water skiing, wind surfing, fishing and many other marine activities.
Batu Cermin Cave is five kilometers from the town of Labuanbajo. It can be reached partly by car, and partly on foot. The grotto is 75 by 75 meters large, and contains stalactites and stalagmites. Some tunnels are narrow and dark but in others sunlight falls.

R U T E NG

Rice field terraces near Ruteng Flores island

Ruteng is the capital of Manggarai Regency that was once ruled by the kings of Bima. The influences of Bima. The influences of Bima and Goa are evident in prevailing titles, such as Karaeng, and in the manner of dress. The shape of the roofs with the buffalo horn symbol, may be an element inherited from the Minangkabau. The cool town of Ruteng lies at the foot of a mountain. It can be reached by air from Kupang or Denpasar via Bima, or by ferry from Bima via Labuanbajo, or from eastern part via Ende and Bajawa. Beside the fame Komodo lizards, the area has many attractions to offer the tourists, such as the caci dance, a wildlife reserve, and archeological caves.
Cancar;Golo Cara; the unique lingko rice fields, circular terraces arranged like a spider web.
Liang Bua: the place where Homo Floresiensis was founded by the archeopathology of new England university of Australia and from Indonesia. The tiny skeleton called Hobbit was discovered during a three-month excavation inside Liang Bua, Scientists believe it may represent a new human species, Homo floresiensis, The species existed alongside modern humans as recently as 13,000 years ago, yet may descend from Homo erectus, which arose some two million years ago.

BAJAWA

Mount Inerie-Ngada-Flores island

 
The capital of Ngada is Bajawa, which lies in the middle of the cool highlands. It is a pleasant little town such as is seldom found elsewhere in Flores. About 135 kilometers from Ruteng all about 5 to 7 hour - driving distance by car, Bajawa can also be reahed from Kupang by air-craft, and from Ende by car.
Abulobo and Inerie are between mountains with sharp peaks known locally as the "sky pillars", and popular among mountaineers. They are located near coast and have wonderful scannery.

B E N A

Bena Traditional village-Ngada Flores island

 
Bena is prototype of an ancient Ngada village. Such villages are found in rather great numbers in the area and can be reached by car from bajawa in about one and half hours. The way of life of the people is unique, and so are the houses and the traditional ceremonies.

R I U N G

Riung Marine Park - 17 Pulau

 
Riung is now wellknown for its seventeen isles that makes the sea surrounding a paradise for marine lovers. Here one can dive, snorkel, and swim.
The beach is a sea-side resort with clear and calm water. There is a beautiful coral reef just off the shore.

ENDE

Kelimutu Crater Lakes - Ende Flores island Indonesia

 
Ende was the site of a kingdom that existed around the end of the 1 8th century. The name today refers to the capital of the Ende regency, which includes the two autonomous territories of Lio and Ende. The people of the area therefore known as Lio Ende people. This town has for many decades been a center of government trade, education and political activity. Rebellion against the Dutch, led by a certain Nipa Do - known as the Wars of Watu Api and Mari Longa - decurred here in 1916 - 1917. And in 1934, the traditionalist leader Soekarno, who was later to become Indonesia's first president, was exiled to Ende by the Dutch colonial government.
The town Ende lies at the foot of mountains lye, lpi, Meja and Wongge. The beautiful bays of Ende, lpi, and Mbuu are favorite sites for beach-site recreation. Ende can be reached by aircraft from Kupang. And also from Denpasar via Bima, or by from Surabaya or Kupang.
The Bung Karno Museum is the old house occupied by Soekarno during his years of exile in Ende. Most of for the old furnishings are still there.
While in exile in Ende, Soekarno wrote and staged few plays, together with the Tonel Kelimutu theatre troupe. Among those plays were Rendorua Ola Nggera Nusa (Rendo That Stirred the Archipelago) and Doctor Satan, a revision on the story of Dr. Frankenstein.
Near the football field in Ende stands an old, big breadfruit tree. Under it, Soekarno often sat, working on political ideas to lead Indonesia towards independence. Those reflections presumably contributed to the opening of the Pancasila concept, which is now the state philosophy of the Indonesian Republic. Just from here was the Pancasila idea born. Today, the Pancasila Birth Monument stand on this precise spot.

KELIMUTU

Kelimutu crater lakes,Ende,Flores island

 
East Nusa Tenggara's natural wonder and one of Indonesia's most mysterious and dramatic sights that can be found on top this mountain, some 66 kilometers from Ende, or 83 kilometers from Maumere. It has a unique and spectacular view on its three crater lakes with their respective colors. The colors, however, have changed continually since the eruption of Mount /ye in Ende in 1969.
The mountain is located at the back of Mount Kelibara, in the Wolowaru District in the Ende, Regency of Central Flores. Keli means mountain and Mutu means boiling. In short, it means volcano. To the local people, this mountain is holy, and a token of God's blessings. It provides fertility to the surrounding lands. It is both heaven and the hell to the people of Lio Ende. Many travelers and scientists, have written about Kelimutu since it was discovered by Van Suchtelen, a Ducth government officer,
in 1915.
Father Bouman published an article in 1929, which made the name Kelimutu known all over the world. Since then, many researchers and tourits have come, as well as the Governor General of Batavia (Jakarta). To get to the lakes, one follows the road, from Moni, then proceed to the crater's top. Near the crater rim was a bungalow, which has now been dismantled.
The presence of the white men, or Ata Bara, was regarded disturbing to the peace of the ancestral spirits. As a result the spirits of Kelimutu disappeared. Earth quakes began rocking the land. Smoke is often released from the crater.
The eruption of 1928 caused many victims and much damage. In 1938 there was another eruption, coming from Tiwu Ata Koo Fai Noo, Ata Nuwa Muri (the Lake of Youth). The biggest took place in 1968, in which the water in the lakes was shot 10 kilometers high into the sky. The peak of Kelimutu itself is 1,690 meters high, and its lake crater I ,410. Other geological data are as follows: Tiwu Ata Polo (the Lake of Evil) has a slopping wall, 150 meters high. The lake is 380 by 280 meters large and 64 meters deep. The volume of the water is about 446,000 cubic meters.
Tiwu Ata Koo Fai Noo and Ata Nawa Muri (the Lake of Youth) has walls 128 meters high. The lake is 430 by 300 square large and 127 meters deep with a water content of about 500.000 cubic meters.
Timu Ata Bupo (the Lake of the old) has twi layers of walls, 240 meters high. The lake covers a surface of 300 by 280 meters high. The water is 67 meters deep and 345,000 cubic meters in volume. The total water content of the three lakes amounts to 1,3 million cubic meters.
In the last three ti five years, the lakes of Kelimutu have changed in color, a phenomenon caused by the geological and chemical processes in the bottom and walls of take lakes. It could also have resulted from changes in the bacteria and micro organism populations due to changes in temperature.
Another theory proposed by village elders, is that there has actually been no change at all, but that the effect is due to optical illusions. To reach Kelimutu can be done by flying to Ende or Maumere, then going by car to Kelimutu.
The surrounding villages are good places serving as bases for visits to Kelimutu, particularly those who wish to have a more leisurely pace and enjoy the views along the road between Ende and maumere, or spend more time in Kelimutu. Those title villages are also known for their excellent weaving all hand made, still use natural dyes.

MAUMERE

Lepo Lerun - weaving ikat - Nita - Maumere

 
A port town on the northeastern coast of Flores and stopover on the way to Ende or to Denpasar, and Ujungpandang, and noted for its good beaches. The bay of Maumere, Waiara, is considered the best diving spot (Flores Marine Resort) as it promise extremely rich marine life.
The resort is a paradise for all divers, underwater photographers, and for everyone interested in marone biology. It has a beautiful sea
garden filled with corals and fish. So does Koka, nearby. Accommodation and facilities for recreation are available.
Ledalero Museum at the outskirts of Maumere has an interesting collection of ethnological objects for the region. Visitors are welcome but advanced arrangements should be made. Ledalero is also a name of a major Catholic Seminary from many of Florinese priest originated.

S I K KA

Weaving ikat,Sikka Natar-Maumere Flores island

 
Sikka was in the past of kingdom, but is is now a regency. The capital is Maumere, on Maumere Bay on the north coast of Flores. The town can be reached by air from Denpasar, Kupang, and Ujungpandang, or by sea from Surabaya, and over land from Ende. Bare mountains and hills dominated the landscape. Today a reforestation program has turned large parts into green pastures.
A prehistoric bronze boat from the Dongsong era, called Dobo or Baobatung is found in a village near Maumere, where it is carefully kept by the people as an ancestral heirloom.
Paga is an old village near the beach. It was a refuge for Catholic missionaries who retreated to this area as the result of pressures by the Dutch authorities in Flores. There is an old well with clear water. Its location is 40 kilometers from Maumere. The small town Nitta was the site of kingdom, and is rich in historical places, traditional ceremonies and beautiful woven clothes with various motifs. It is located 10 kilometers from Maumere.
Sikka-Lela are the viliges which were formerly center from which the Roman Catholic religion spread across Flores. An old well, dug by the priest Le Cocg (1885), can still be found. Bola Beach is located in the southern past of Flores near Sikka and Lela. Many historical relies are found in these two areas, ranging from traditional houses, to rare ivory heirlooms. Ivory was in the past use as a dowry in marriage. Some of the villages in Sikka, such as Sikka, Lela and Nita produce beautiful ikat textiles with motifs that are peculiar to the region.
Like TanaKa, in Ende the soil covering hill near Lakebai is also edible. The grains of earth can be eaten after they are fried.
 

The island of Palue, in the north of Flores has a megalithic culture. In the front- yard of houses lie the graves and "mezbah" offering stones. The people of the area are known to make great sailors. Life is still much influenced by the belief in spirits, which are believed to reside in natural objects. The island can be reached in a few hours by motorboat from the Maumere prier.

Lake Kelimutu Flores Indonesia

LAKE KELIMUTU

East Nusa Tenggara's natural wonder and one of Indonesia's most mysterious and dramatic sights that can be found on top this mountain, some 66 kilometers from Ende, or 83 kilometers from Maumere. It has a unique and spectacular view on its three crater lakes with their respective colors. The colors, however, have changed continually since the eruption of Mount /ye in Ende in 1969.
The mountain is located at the back of Mount Kelibara, in the Wolowaru District in the Ende, Regency of Central Flores. Keli means mountain and Mutu means boiling. In short, it means volcano. To the local people, this mountain is holy, and a token of God's blessings. It provides fertility to the surrounding lands. It is both heaven and the hell to the people of Lio Ende. Many travelers and scientists, have written about Kelimutu since it was discovered by Van Suchtelen, a Ducth government officer,
in 1915
Father Bouman published an article in 1929, which made the name Kelimutu known all over the world. Since then, many researchers and tourits have come, as well as the Governor General of Batavia (Jakarta). To get to the lakes, one follows the road, from Moni, then proceed to the crater's top. Near the crater rim was a bungalow, which has now been dismantled.
The presence of the white men, or Ata Bara, was regarded disturbing to the peace of the ancestral spirits. As a result the spirits of Kelimutu disappeared. Earth quakes began rocking the land. Smoke is often released from the crater.
The eruption of 1928 caused many victims and much damage. In 1938 there was another eruption, coming from Tiwu Ata Koo Fai Noo, Ata Nuwa Muri (the Lake of Youth). The biggest took place in 1968, in which the water in the lakes was shot 10 kilometers high into the sky. The peak of Kelimutu itself is 1,690 meters high, and its lake crater I ,410. Other geological data are as follows: Tiwu Ata Polo (the Lake of Evil) has a slopping wall, 150 meters high. The lake is 380 by 280 meters large and 64 meters deep. The volume of the water is about 446,000 cubic meters.
Tiwu Ata Koo Fai Noo and Ata Nawa Muri (the Lake of Youth) has walls 128 meters high. The lake is 430 by 300 square large and 127 meters deep with a water content of about 500.000 cubic meters.
Timu Ata Bupo (the Lake of the old) has twi layers of walls, 240 meters high. The lake covers a surface of 300 by 280 meters high. The water is 67 meters deep and 345,000 cubic meters in volume. The total water content of the three lakes amounts to 1,3 million cubic meters.
In the last three ti five years, the lakes of Kelimutu have changed in color, a phenomenon caused by the geological and chemical processes in the bottom and walls of take lakes. It could also have resulted from changes in the bacteria and micro organism populations due to changes in temperature.
Another theory proposed by village elders, is that there has actually been no change at all, but that the effect is due to optical illusions. To reach Kelimutu can be done by flying to Ende or Maumere, then going by car to Kelimutu
The surrounding villages are good places serving as bases for visits to Kelimutu, particularly those who wish to have a more leisurely pace and enjoy the views along the road between Ende and maumere, or spend more time in Kelimutu. Those title villages are also known for their excellent weaving all hand made, still use natural dyes.

Lake Kelimutu Flores Indonesia

Kelimutu is a volcano, close to the town of Moni in central Flores Island of Indonesia containing three summit crater lakes of varying colors. Tiwu Ata Mbupu (Lake of Old People) is usually blue and is the westernmost of the three lakes. The other two lakes, Tiwu Nuwa Muri Koo Fai (Lake of Young Men and Maidens) and Tiwu Ata Polo (Bewitched or Enchanted Lake) are separated by a shared crater wall and are typically green or red in color, respectively. The lake colors do vary on a periodic basis. Subaqueous fumaroles are the probable cause of active upwelling that occurs at the two eastern lakes.[1]
The lake have been a source of minor phreatic eruptions in historical time. The summit of the compound 1639-m-high Kelimutu volcano is elongated two km in a WNW-ESE direction; the older cones of Kelido and Kelibara are located respectively three km to the north and two km to the south. The scenic lakes are a popular tourist destination. Keli Mutu is also of interest to geologists because the three lakes are different colors yet reside at the crest of the same volcano [2].
The closest airports are Maumere, and Ende. There are regular flights to Maumere from Bali.
The drive from Maumere to Moni, the town at the base of Keli Mutu, takes about 3 hours.

Indonesian setting
Indonesia is one of the world's most geologically active countries. Given its combination of active volcanism and tropical climate, it is home to several volcanoes which exemplify the type of dynamic interactions between the forces of the endosphere and exosphere that are characteristic of volcanic lake environments. Of all the volcanos in Indonesia, Keli Mutu on the island of Flores appears to have the most exotic lakes. In fact, its lakes are so brightly colored that they are featured on the 5,000 rupiah bill and thought of as a national treasure by the people of Indonesia.
Located between Malaysia and Australia, the islands comprising the approximately 3,000 mile long latitudinal axis of Indonesia are the physical expression of the subduction of the Indo-Australian plate to the south beneath the Eurasian plate to the north. Typical features of such "island arcs" are andesitic stratovolcanoes. These volcanoes may either be 1) well-developed lofty cones (e.g. Merapi in central Java) or 2) complex structures featuring mutiple craters and irregular moonscape summits sculpted by alternate periods of building up and destruction (e.g. Una-Una in Celebes) (Umbgrove, 1949). The active stratovolcanoes of Indonesia are particularly well known for their highly explosive eruptions, devastating lahars (mud-flows), and associated tsunami waves. Currently there are more than 200 active and many more extinct volcanoes present in Indonesia.
Because Indonesia straddles the equator it does not have temperature-defined seasons. The year-round average monthly temperature is ~80 deg F and the average rainfall is ~3 m/year (Ulack & Pauer, 1989). Those islands that deviate to the north or south of the equator may experience monsoons, while those that are closer to Australia are subject to a more pronounced dry season. Where present, the dry season spans from August through part of October and is immediately followed by a wet season that eventually winds down in March. Striking seasonal variations in precipitation along the latitudinal axis of Indonesia were first described by the naturalist George Wallace (co-founder of the theory of evolution by natural selection) in the mid 1800's.
Keli Mutu Setting
Keli Mutu is a passively degassing stratovolcano (Fig.1) capped by three crater lakes (Fig. 2) containing exotic fluids and whose physico-chemical expressions have changed dramatically through the years. The volcano is located on Flores, an island along the Lesser Sunda islands chain of Indonesia. An early description of Keli Mutu was provided by the French naturalist LeRoux, who mentions it in his travel log of eastern Indonesia in 1896. A more comprehensive geologic and topographic survey was performed in the 1920's by the Dutch colonial geologist Kemmerling, who traveled through Flores on horseback and early motor vehicle. Since 1929 no publicly reported systematic survey of Flores has been done using modern techniques. A map of Flores (TPC N-12BG) was published in 1972 as part of the World Aeronautical Chart (WAC) series, but the topographic information is sketchy.
Keli Mutu Crater Lakes
Three crater lakes are located on the eastern summit of Keli Mutu. Each of the lakes has a distinctive physical structure, a unique geochemical and hydrothermal regime, and a particular historical sequence of color changes controlled by changes in physico-chemical conditions.
Tiwu Ata Polo (TAP), the "enchanted lake", lies on the southeastern side of the volcanic peak (Fig.3). A thermal plume in the northwest part of the lake indicates underlying subaerial fumarolic or hydrothermal activity. A white froth is present on the lake's surface around the plume when the convective activity momentarily increases. Rock debris is often carried into TAP during rainstorms by water draining the volcano summit around the lake. Two peaks abutting the crater rim help stabilize the east and northeast crater wall, while further around to the southeast a dip suggests a possible one-time overflow outlet. Such an outlet would have fed the river Ria Mbuli, whose upland source is in that area.
Tiwu Nua Muri Koohi Fah (TiN), the "lake of young men and maidens", is adjacent to TAP and is the deepest lake (Fig.4). A sizable tear in the western wall was the location of a pre-1929 breaching and overflow event. Visible fumarolic activity above the shoreline of TiN was reported by Kemmerling, but this activity has declined and is no longer present. Subaerial fumarolic or hydrothermal activity is implied by a large thermal plume in the center of the lake which slowly convects the water. A fresh supply of yellow froth (probably the same type of elemental sulfur found in the "cool acid-brine" crater lake at Kawa Ijen) is brought up by the plume and pushed out toward the crater wall. A particularly large cover of this froth has accumulated at the base of the north wall (Fig.4). During rainstorms the froth is scattered by inflowing water and landslides, though some of it may be disappearing altogether.
TAP and TiN are only separated by a steep parabolic partition that arcs down to a minimum height of ~35m above the surface level of the lakes (Fig.3). According to Kemmerling this separating wall was as high as the surrounding crater rim 70 years before his survey, but it had subsequently eroded down by the time of his visit (Kemmerling, 1929). Recent unconfirmed reports (1996) state that the partition has crumbled and the lakes are now mingled. A directory of volcanoes published by the Smithsonain Institute lists moderate "hydrothermal blasts" of TiN that occured in 1938 and again in 1965. Each of these events was reported to have lasted longer than a month but was small and confined to the crater (Simkin et al, 1981).
Tiwu Ata Mbupu (TAM), the "lake of elders", is the western-most lake (Fig. 5). TAM is structurally different from the other two in that the pit crater it is in is itself located in the center of a larger crater. Kemmerling reported both aerial and subaerial fumarolic activity for the TAM crater, but none was observed in 1992. Small landslides constantly add to the steep rubble slopes along the lake's shore, and large boulders periodically drop into the lake. TAM's shoreline is coated with a film colored in different shades of red, orange, and yellow depending on how thick it is. Gypsum crystals grow in the cracks of the crater wall in the first few meters above the prosent water surface.
Research at Keli Mutu
Geochemical surveys and subsequent analyses of the lakes on Keli Mutu have been carried out recently by scientists from Wesleyan University (Middletown, CT, USA). Results have been published in
Pasternack, G.B. (1993) Acid-brine crater lakes: a case study. Undergraduate senior thesis, Wesleyan University, 160 pp.
Pasternack, G.B. and Varekamp, J.C. (1994) The geochemistry of the Keli Mutu crater lakes, Flores, Indonesia, Geochemical Journal 28:243-262.
reprint requests to: gpast@jhu.edu
The work involved describing the chemistry of each lake, interpreting the chemistries in terms of water-rock interactions and volcanic fluxes, and deriving a physical lake model that delineates the parameter-window for volcanic crater lake existence.
Geochemical investigation of the vertical and lateral compositions of the lakes on Keli Mutu required the use of a remote sampling system. Lake temperature, pH, and dissolved oxygen content were determined in the field, while the analytical chemistries of lake fluids and sediments were determined in the months after the expedition to Keli Mutu. To reconstruct the in situ chemistries of the lakes' aqueous systems, a solution equilibrium modeling program (SOLVEQ) was applied.
The primary conclusion of the work at Keli Mutu is that the three Keli Mutu lakes are all fed by a similar volcanic gas source, but as a result of the mediated subaqueous transport of that gas it yields different chemical "expressions" in each crater lake. Specific findings include the following:
• Tiwu Ata Polo (TAP) is an intermediate "acid-saline" volcanic crater lake whose frequent color changes are probably the direct result of changes in the oxidation state of the lake's water. TAP is intermediate in volcanic activity relative to the other Keli Mutu lakes.
• Tiwu Nua Moori Koohi Fah (TiN) is a "cool acid-brine" volcanic crater lake that contains exotic sulfur compounds and probably a host of copper-rich minerals in the sediments. Of the three Keli Mutu lakes, TiN is presently experiencing the greatest fumarolic input, which may include a flux of ~85 tonnes of sulfur dioxide per day (~55MW energy output).
• Tiwu Ata Mbupu (TAM) is an "acid-sulfate" volcanic crater lake whose gaseous input is presently very small relative to those for the other Keli Mutu lakes. In the 1970s it appears that TAM was much more active than it presently is.
• Comparison of the individual lakes with their respective historic chemistries demonstrates that they are all approaching chemical steady state.
• Several seepage outlets exist on and around Keli Mutu. The river Watu Gana bears a strong TAP fluid signature, but other hydrothermal waters show no crater lake signature at all.
________________________________________
Info for Keli Mutu Tourists
Many Indonesian guidebooks describe the vibrant colors of the Keli Mutu lakes as resulting from the minerals in the lakes. While this is partly correct, the most important determinant of color in the lakes is oxygen. Just like your blood, when the lake waters lack oxygen they look green (look at your wrist). Conversely, when they are rich in oxygen, they are a deep red to black. Obviously this is oversimplifying matters a little, but the point is that you should not be misled... Contrary to guidebook authors claims (which aim to increase drama, mystery, suspense, etc), scientists do in fact understand why the lakes looks like they do.
________________________________________
Back to Volcanic Lakes or Greg Pasternack's Research