Monday, November 16, 2015

Derawan Islands


The Derawan Islands are in the province of East Kalimantan in Indonesia. They include Derawan, Sangalaki, Kakaban, Maratua, Panjang, and Samama Island and submerged reefs and islets. They are located in the Sulawesi Sea, on the coastal shelf of East Kalimantan (2°17′N - 118°13′E). The islands are part of the Berau Regency.

Biodiversity
Derawan islands is a part of Coral Triangle, which contains one of the richest marine biodiversity on earth. Located in a biodiversity hotspot, the Derawan Islands feature 872 species of reef fishes, 507 species of coral, and invertebrates, including protected species (5 giants clam species, 2 sea turtles, coconut crab, etc.). Some of the islands harbor the heavily exploited turtle eggs and yet the largest green turtle nesting site in Indonesia.

Unpoisoned jellyfish
Derawan Islands have at least two ponds contain unpoisoned jellyfish, one in Kakaban Island and the other in Maratua Island with Haji Buang Pond. Kakaban is more famous than the second which is also more difficult to access. Indonesia at least have 7 ponds with unpoisoned jellyfish, the others are 3 ponds in Raja Ampat, West Papua, one in Togean Island, Central Sulawesi and one in Rote Island, East Nusa Tenggara.

Resources Use
There are two inhabited islands, namely Derawan (1 village of 1,259 people) and Maratua (4 villages of 2,704 people). Fishing is an important income-generating activity for the community. Since the early 1990s, people have caught live groupers, napoleon wrasse, and lobsters, to fill high demand. There are 3 dive resorts on Derawan Islands, while more additional resorts or facilities are in the planning process.

Caves
Maratua Island is 384.36 square kilometers and has at least 13 caves, but the prediction, more than a hundred caves are not yet explored. The caves usually have connection directly to the sea due to the caves are originated from the reef which sea water infiltrates into the land making underground channels.

Airport and seaport
To boost tourism, local government will build an airport and a seaport at Maratua Island and both were predicted to operate in 2013. World Wildlife Fund and environmental activists are opposing it because the construction of the projects will surely affect the turtle habitat and coral reefs on Maratua Island, but the local government apparently focuses more on development projects instead of conservation.

Mount Bromo


Mount Bromo is an active volcano and part of the Tengger massif, in East Java, Indonesia. At 2,329 metres (7,641 ft) it is not the highest peak of the massif, but is the most well known. The massif area is one of the most visited tourist attractions in East Java, Indonesia. The volcano belongs to the Bromo Tengger Semeru National Park. The name of Bromo derived from Javanese pronunciation of Brahma, the Hindu creator god. Sulfur is collected from inside the caldera by workers.
Mount Bromo sits in the middle of a vast plain called the "Sea of Sand" (Javanese: Segara Wedi or Indonesian: Lautan Pasir), a protected nature reserve since 1919. The typical way to visit Mount Bromo is from the nearby mountain village of Cemoro Lawang. From there it is possible to walk to the volcano in about 45 minutes, but it is also possible to take an organised jeep tour, which includes a stop at the viewpoint on Mount Penanjakan (2,770 m or 9,088 ft) (Indonesian: Gunung Penanjakan). The viewpoint on Mount Penanjakan can also be reached on foot in about two hours.
Depending on the degree of volcanic activity, the Indonesian Centre for Volcanology and Disaster Hazard Mitigation sometimes issues warnings against visiting Mount Bromo.

Culture
On the fourteenth day of the Hindu festival of Yadnya Kasada, the Tenggerese people of Probolinggo, East Java, travel up the mountain in order to make offerings of fruit, rice, vegetables, flowers and sacrifices of livestock to the mountain gods by throwing them into the caldera of the volcano. The origin of the ritual lies in the 15th century legend where a princess named Roro Anteng started the principality of Tengger with her husband, Joko Seger. The couple were childless and therefore beseeched the assistance of the mountain gods. The gods granted them 24 children but stipulated that the 25th child, named Kesuma, must be thrown into the volcano as a human sacrifice. The gods' request was implemented. The tradition of throwing sacrifices into the volcano to appease these ancient deities continues today and is called the Yadnya Kasada ceremony. Though fraught with danger, some locals risk climbing down into the crater in an attempt to recollect the sacrificed goods that they believe could bring them good luck.
On the Segara Wedi sand plain sits a Hindu temple called Pura Luhur Poten. The temple holds a significant importance to the Tenggerese scattered across the mountain villages, such as Ngadisari, Wonokitri, Ngadas, Argosari, Ranu Prani, Ledok Ombo and Wonokerso. The temple organises the annual Yadnya Kasada ceremony which lasts for about one month. On the 14th day, the Tenggerese congregate at Pura Luhur Poten to ask for blessings from Ida Sang Hyang Widi Wasa and the God of Mahameru (Mount Semeru). Then the crowd proceeds along the crater edges of Mt Bromo where offerings are thrown into the crater. The major difference between this temple and Balinese ones are the type of stones and building materials. Pura Luhur Poten uses natural black stones from volcanoes nearby, while Balinese temples are mostly made from red bricks. Inside this pura, there are several buildings and enclosures aligned in a mandala zone composition.

Activity
2004 eruptions
Mount Bromo erupted in 2004. That eruptive episode led to the death of two people who had been hit by rocks from the explosion.
2010 eruptions
On Tuesday, 23 November 2010, 16.30 WIB (Western Indonesian Time), the Indonesian Centre of Vulcanology and Geology Hazard Mitigation (CVGHM) confirmed the activity status of Mount Bromo at "alert" due to increasing tremor activity and shallow volcanic earthquakes at the mountain. Concerns were raised that a volcanic eruption might be likely to occur. As a precaution local residents and tourists were instructed to remain clear of an area within a radius of three kilometres from the caldera and refugee encampments were erected. The area surrounding the Teggera caldera of Bromo remained off-limits for visitors throughout the remainder of 2010.
Bromo started to erupt ash on Friday 26 November 2010.
On 29 November 2010 Transport Ministry spokesman Bambang Ervan announced that Malang's domestic airport would be closed until 4 December 2010. Malang is a city of about 800,000 people is about 25 km (16 mi) west of Mount Bromo. Abdul Rachman Saleh Airport normally handles 10 daily domestic flights from the capital Jakarta. Government volcanologist Surono reported that the volcano was spitting columns of ash some 700 metres (2,300 feet) into the sky.

Mount Rinjani



Mount Rinjani or Gunung Rinjani is an active volcano in Indonesia on the island of Lombok. Administratively the mountain is in the Regency of North Lombok, West Nusa Tenggara (Indonesian: Nusa Tenggara Barat, NTB). It rises to 3,726 metres (12,224 ft), making it the second highest volcano in Indonesia.
On the top of the volcano is a 6-by-8.5-kilometre (3.7 by 5.3 mi) caldera, which is filled partially by the crater lake known as Segara Anak or Anak Laut (Child of the Sea) due to blue color of water lake as Laut (Sea). This lake is approximately 2,000 metres (6,600 ft) above sea level and estimated to be about 200 metres (660 ft) deep; the caldera also contains hot springs. Sasak tribe and Hindu people assume the lake and the mount are sacred and some religious activities are occasionally done in the two areas. On 31 October 2015, Mount Rinjani started erupting again.

Geography
Lombok is one of the Lesser Sunda Islands, a small archipelago which, from west to east, consists of Bali, Lombok, Sumbawa, Flores, Sumba and the Timor islands; all are located at the edge of the Australian continental shelf. Volcanoes in the area are formed due to the action of oceanic crusts and the movement of the shelf itself. Rinjani is one of at least 129 active volcanoes in Indonesia, four of which belong to the volcanoes of the Sunda Arc trench system forming part of the Pacific Ring of Fire – a section of fault lines stretching from the Western Hemisphere through Japan and South East Asia. The islands of Lombok and Sumbawa lie in the central portion of the Sunda Arc. The Sunda Arc is home to some of the world's most dangerous and explosive volcanoes. The eruption of nearby Mount Tambora on Sumbawa is known for the most violent eruption in recorded history on 15 April 1815, with a scale 7 on the VEI.
The highlands are forest clad and mostly undeveloped. The lowlands are highly cultivated. Rice, soybeans, coffee, tobacco, cotton, cinnamon, cacao, cloves, cassava, corn, coconuts, copra, bananas and vanilla are the major crops grown in the fertile soils of the island. The slopes are populated by the indigenous Sasak population. There are also some basic tourist related activities established on Rinjani primarily in or about the village of Senaru.
Rinjani volcano on the island of Lombok rises to 3,726 metres (12,224 ft), second in height among Indonesian volcanoes only to Sumatra's Kerinci volcano. Rinjani has a steep-sided conical profile when viewed from the east, but the western side of the compound volcano is truncated by the 6 x 8.5 km, oval-shaped Segara Anak caldera. The western half of the caldera contains a 230-metre-deep lake whose crescentic form results from growth of the post-caldera cone Barujari at the eastern end of the caldera.

Geologic summary
On the basis of plate tectonics theory, Rinjani is one of the series of volcanoes built in the Lesser Sunda Islands due to the subduction of Indo-Australian oceanic crust beneath the Lesser Sunda Islands, and it is interpreted that the source of melted magma is about 165–200 kilometres (103–124 mi) depth.
The geology and tectonic setting of Lombok (and nearby Sumbawa) are described as being in the central portion of the Sunda Arc. The oldest exposed rocks are Miocene, suggesting that subduction and volcanism began considerably later than in Java and Sumatra to the west, where there are abundant volcanic and intrusive rocks of Late Mesozoic age. The islands are located on the eastern edge of the Sunda shelf, in a zone where crustal thickness is apparently rapidly diminishing, from west to east.
The seismic velocity structure of the crust in this region is transitional between typical oceanic and continental profiles and the Mohorovičić discontinuity (Moho) appears to lie at about 20 kilometres (12 mi) depth. These factors tend to suggest that there has been limited opportunity for crustal contamination of magmas erupted on the islands of Lombok and Sumbawa. In addition, these islands lie to the west of those parts of the eastern-most Sunda and west Banda arcs where collision with the Australian plate is apparently progressing.
The volcano of Rinjani is 165 to 190 kilometres (103–118 mi) above the Benioff Zone. There is a marked offset in the line of active volcanoes between the most easterly Sumbawa volcano (Sangeang Api) and the line of active volcanoes in Flores. This suggests that a major transcurrent fault cut across the arc between Sumbawa Island and Flores. This is considered to be a feature representing a major tectonic discontinuity between the east and west Sunda Arcs (the Sumba Fracture). Further, a marked absence of shallow and intermediate earthquake activity in the region to the south of Lombok and Sumbawa is a feature interpreted to represent a marked break in the Sunda Arc Zone. Faulting and folding caused strong deformation in the eastern part of Lombok Basin and is characterized by block faulting, shale diapirs and mud volcano.

Volcanology
The Rinjani caldera forming eruption is thought to have occurred in the 13th century. Dated to "late spring or summer of 1257," this eruption is now considered the likely source of high concentrations of sulfur found in widely dispersed ice core samples and may have been "the most powerful volcanic blast since humans learned to write." The massive eruption may have triggered an episode of global cooling and failed harvests.
Eruption rate, eruption sites, eruption type and magma composition have changed during the last 10,000 years before the caldera forming eruption. The eruptions of 1994 and 1995 have presented at Gunung Baru (or 'New Mountain' - approximately 2,300 metres (7,500 ft) above sea level) in the center of this caldera and lava flows from subsequent eruptions have entered the lake. This cone has since been renamed Gunung Barujari (or 'Gunung Baru Jari' in Indonesian).
The first historical eruption occurred in September 1847. The most recent eruption of Mount Rinjani was in May 2010 and the most recent significant eruptions occurred during a spate of activity from 1994 to 1995 which resulted in the further development of Gunung Barujari. Historical eruptions at Rinjani dating back to 1847 have been restricted to Barujari cone and the Rombongan dome (in 1944) and consist of moderate explosive activity and occasional lava flows that have entered Segara Anak lake. The eruptive history of Rinjani prior to 1847 is not available as the island of Lombok is in a location that remained very remote to the record keeping of the era.
On 3 November 1994, a cold lahar (volcanic mudflow) from the summit area of Rinjani volcano traveled down the Kokok Jenggak River killing thirty people from the village of Aikmel who were caught by surprise when collecting water from the river in the path of the flow.
In connection with the eruption of the cone Gunung Barujari the status for Gunung Rinjani has been raised from Normal (VEI Level 1) to 'be vigilant' (VEI Level 2) since May 2, 2009 . In May 2010 Gunung Rinjani was placed in the standby status by Center for Volcanology & Geological Hazard Mitigation, Indonesia with a recommendation that there be no activity within a radius of 4 kilometres (2.5 mi) from the eruption at Gunung Barujari.

Maluk Beach


Maluk Beach is one of stunning beaches in Sumbawa Island. The color of the sun will change becomes golden gradually at sunset, and it will give beautiful panorama. You can just relax or sit on fine sand while shipping your tea. Just like other beaches in Indonesia, it has white and soft sand. The pristine water seems invite you to swim or snorkel. Enjoying the wave of water is also one of attractive thing you can do when you visit the beach. For most surfers, the wave of Maluk is powerful and strong.

Location
Maluk Beach is located at a peninsula. Precisely, the beach is situated at Maluk Jereweh Village, West Sumbawa Regency, West Nusa Tenggara, Indonesia. Because the beach is flanked by two hills, Mantun Hill at the north, and Balas Hill at the south, it makes Maluk has wonderful panorama. You can start you journey from Benete Terminal. You can hire a motorcycle, take ojek to Maluk beach. You only need to pay IDR2,000 or US$0.2.
The cost is cheap because you only need to go for 1.5 km. Differently, if you want to hire a motorcycle, you only need to pay IDR100,000 per day, or US$10. By hiring a motorcycle, you will be free and have more time to get more spots in Maluk Beach. The good thing about Maluk Beach is you don’t need to buy a ticket.


Activities
There are many things you can do when you visiting Maluk Beach. First, you can see conservation of turtle. In this place, you will see the eggs of turtles, or even the baby of turtle. If you lucky, you can release the baby of turtle into the beach. However, the most favorite activity in the beach is surfing. Surfers from around the world love the wave in the beach because it is strong and powerful, especially when the tide is high.
The high of wave can be 4 – 6 meters. If you want to challenge your adrenaline, this is one of thing you can do in Maluk Beach. But, if you want to relax and enjoy the day, you can just lie down on white sand. From the distance, you can see other visitors canoeing or swimming.
There are many food stalls offering sea food along the beach. The traditional culinary around here is special because it made by traditional ingredients. As the source of seafood, fishermen provide fresh fishes, lobsters, and crabs. The most favorite dish is named as spicy dendeng.


According the report of local government, West Sumbawa has dozens of surfing spots. Even, there are surfers gave three names main beaches, i.e. Sekongkang, Maluk and Njlenga. These spots are well known as golden triangle. That is mean the real surfers should visit these surfing spots. With those qualities, that makes the three of these beaches become the spot of international competition of surfing. The participants come from many countries, such as Philippine, Australia, New Zealand, and Indonesia.

Accommodations
The facilities and accommodations in Maluk Island are complete. There are many home stay and hostel. These guesthouses are simple you can rest while accompanied by sound of water at night.
Or, you can start the journey from Mataram – Lombok. Then, you can continue to the port to cross the sea for 22 km. You have to wait a ferry and it will take around 2 hours to arrive at Poto Tano Port in West Sumbawa. If you want to go to Taliwang and Njlenga, it will take 2.5 hours, and to Maluk Beach, it will take 3.5 hours.

Thursday, November 5, 2015

Lake Toba


Lake Toba  is a large natural lake occupying the caldera of a supervolcano. The lake is about 100 kilometres long, 30 kilometres wide, and up to 505 metres (1,666 ft) deep. Located in the middle of the northern part of the Indonesian island of Sumatra, with a surface elevation of about 900 metres (2,953 ft), the lake stretches from 2.88°N 98.52°E to 2.35°N 99.1°E. It is the largest lake in Indonesia and also the largest volcanic lake in the world.

Lake Toba is the site of a massive supervolcanic eruption estimated at VEI 8 that occurred 69,000 to 77,000 years ago, representing a climate-changing event. It is the largest known explosive eruption on Earth in the last 25 million years. According to the Toba catastrophe theory, it had global consequences for human populations: it killed most humans living at that time and is believed to have created a population bottleneck in central east Africa and India, which affects the genetic make up of the human world-wide population to the present.

It has been accepted that the eruption of Toba led to a volcanic winter with a worldwide decrease in temperature between 3 to 5 °C (5.4 to 9.0 °F), and up to 15 °C (27 °F) in higher latitudes. Additional studies in Lake Malawi in East Africa show significant amounts of ash being deposited from the Toba eruptions, even at that great distance, but little indication of a significant climatic effect in East Africa.

Geology
The Toba caldera complex in Northern Sumatra, comprises four overlapping volcanic craters that adjoin the Sumatran "volcanic front." The fourth and youngest caldera is the world's largest Quaternary caldera (100 by 30 km (62 by 19 mi)) and intersects the three older calderas. An estimated 2,800 km3 (670 cu mi) of dense-rock equivalent pyroclastic material, known as the youngest Toba tuff, was released during one of the largest explosive volcanic eruptions in recent geological history. Following this eruption, a resurgent dome formed within the new caldera, joining two half-domes separated by a longitudinal graben.

At least four cones, four stratovolcanoes, and three craters are visible in the lake. The Tandukbenua cone on the northwestern edge of the caldera has only sparse vegetation, suggesting a young age of several hundred years. Also, the Pusubukit (Hill Center) volcano (1971 metres above sea level) on the south edge of the caldera is solfatarically active and is a Geology Sanctuary.

Flora and fauna
The flora of the lake includes various types of phytoplankton, emerged macrophytes, floating macrophytes, and submerged macrophytes, while the surrounding countryside is rainforest including areas of Sumatran tropical pine forests on the higher mountainsides.

The fauna includes several species of zooplankton and benthic animals. Since the lake is oligotrophic (nutrient-poor), the native fish fauna is relatively scarce, and the only endemics are Rasbora tobana (strictly speaking near-endemic, since also found in some tributary rivers that run into the lake) and Neolissochilus thienemanni, locally known as the Batak fish. The latter species is threatened by deforestation (causing siltation), pollution, changes in water level and the numerous fish species that have been introduced to the lake. Other native fishes include species such as Aplocheilus panchax, Nemacheilus pfeifferae, Homaloptera gymnogaster, Channa gachua, Channa striata, Clarias batrachus, Barbonymus gonionotus, Barbonymus schwanenfeldii, Danio albolineatus, Osteochilus vittatus, Puntius binotatus, Rasbora jacobsoni, Tor tambra, Betta imbellis, Betta taeniata and Monopterus albus. Among the many introduced species are Anabas testudineus, Oreochromis mossambicus, Oreochromis niloticus, Ctenopharyngodon idella, Cyprinus carpio, Osphronemus goramy, Trichogaster pectoralis, Trichopodus trichopterus, Poecilia reticulata and Xiphophorus hellerii.

More recent activity
Since the major eruption ~70,000 years ago, eruptions of smaller magnitude have also occurred at Toba. The small cone of Pusukbukit formed on the southwestern margin of the caldera and lava domes. The most recent eruption may have been at Tandukbenua on the northwestern caldera edge, suggested by a lack of vegetation that could be due to an eruption within the last few hundred years.

Some parts of the caldera have shown uplift due to partial refilling of the magma chamber, for example, pushing Samosir Island and the Uluan Peninsula above the surface of the lake. The lake sediments on Samosir Island show that it has risen by at least 450 m (1,476 ft) since the cataclysmic eruption. Such uplifts are common in very large calderas, apparently due to the upward pressure of below-ground magma. Toba is probably the largest resurgent caldera on Earth. Large earthquakes have recently occurred in the vicinity of the volcano, notably in 1987 along the southern shore of the lake at a depth of 11 km (6.8 mi). Such earthquakes have also been recorded in 1892, 1916, and 1920–1922.

Lake Toba lies near the Great Sumatran fault, which runs along the centre of Sumatra in the Sumatra Fracture Zone. The volcanoes of Sumatra and Java are part of the Sunda Arc, a result of the northeasterly movement of the Indo-Australian Plate, which is sliding under the eastward-moving Eurasian Plate. The subduction zone in this area is very active: the seabed near the west coast of Sumatra has had several major earthquakes since 1995, including the 9.1 2004 Indian Ocean earthquake and the 8.7 2005 Sumatra earthquake, the epicenters of which were around 300 km (190 mi) from Toba.

Wednesday, August 5, 2015

Bunaken National Park


The Bunaken National Park is a marine park in the north of Sulawesi island, Indonesia. The park is located near the centre of the Coral Triangle, providing habitat to 390 species of coral as well as many fish, mollusc, reptile and marine mammal species. The Park is representative of Indonesian tropical water ecosystems, consisting of seagrass plain, coral reef, and coastal ecosystems.

It was established as a national park in 1991 and is among the first of Indonesia's growing system of marine parks. It covers a total area of 890.65 km², 97% of which is marine habitat. The remaining 3% of the park is terrestrial, including the five islands of Bunaken, Manado Tua, Mantehage, Nain and Siladen. The southern part of the Park covers part of the Tanjung Kelapa coast.

Geology

North Sulawesi is considered to be a 'young' formation, of 5-24 million years of age. The region has undergone explosive volcanism 1.5-5 million years ago, which resulted in the volcanic tuff that characterizes the existing topography. Manado Tua is an inactive volcano formed in a classical cone shape and rising over 600 m above sea level, the highest elevation in the park. Bunaken Island also has volcanic origins with a significant amount of uplifted fossil coral. Nain Island is also a dome-shaped island, 139m in height. Mantehage Island is relatively flat and seems to be sinking into the sea. The island has extensive mangrove forest flats, partially separated by saltwater channels. Siladen is a low-lying coral sand island with no significant topography. Arakan-Wawontulap and Molas-Wori on the mainland of North Sulawesi are relatively flat areas at the base of volcanic hills. The absence of a continental shelf allows the coastal area of the park to drop directly down the continental slope. The sea depth between the islands of the park is 200 to 1,840 metres.

Flora and fauna

A very rich coral ecosystem covers most of Bunaken National Park, dominated by fringing reef and barrier reef corals. There are about 390 species of coral recorded in the waters of the Park. A distinct feature is a 25-50 metre vertical coral wall which is inhabited by 13 coral genus. The seaweeds that can be found here include Caulerpa, Halimeda, and Padina species, while the dominant seagrasses, in particular in the islands of Montehage and Nain, are Thalassia hemprichii, Enhallus acoroides, and Thalassodendron ciliatum. The park is also abundant in different species of fish, marine mammals and reptiles, birds, molluscs and mangrove species.

About 90 species of fish live in the waters of the park, among them being the Emperor Angelfish, Almaco Jack, Spotted Seahorse, Bluestripe Snapper, Pinkish Basslet and Two-lined monocle bream. The species of mollusc include the Giant Clam, Horned Helmet Shells, Chambered Nautilus, and ascidians.

It is claimed that this park has seven times more genera of coral than Hawaii, and more than 70% of all the known fish species of the Indo-Western Pacific.

On land, the islands are rich in species of palm, sago, woka, silar and coconut. Among the animal species that live on the land and the beaches are Celebes crested macaque, Timor Deer, and Sulawesi bear cuscus. The mangrove forest of the Park contains, among others Rhizophora and Sonneratiaspecies. This forest is also rich in species of crab, lobster, mollusc, and sea birds such as gulls, herons, sea doves, and storks.

Human habitation and tourism

The area is densely populated, with 22 villages inside the park comprising about 35,000 people. Most locals work as fishermen or farmers cultivating coconut, sweet potato, banana or seaweed for export, while a small number are employed in tourism as dive guides, boat operators and cottage staff. Tourism is strongly developed, with accommodation ranging from backpacker cottages to 5 star resorts. Between 2003 and 2006 the number of visitors ranged from 32,000 to 39,000 of which 8-10,000 were international visitors.

Conservation and threats

Bunaken National Park was formally established in 1991 and is among the first of Indonesia's marine parks. In 2005 Indonesia submitted an application to UNESCO for including the park on the World Heritage List. Despite its national park status and significant funding, the park has suffered a slow, continuous degradation due to a number of threats including coral mining, anchor damage, blast fishing, cyanide fishing, diving, and trash. The World Wildlife Fund provides conservation support in the National Park as part of the Sulu Sulawesi Marine Eco-region Action Plan. This includes participatory enforcement and patrol, which resulted in significant reduction of blast fishing.

Borobudur


Borobudur, or Barabudur, is a 9th-century Mahayana Buddhist Temple in Magelang, Central Java, Indonesia. The monument consists of nine stacked platforms, six square and three circular, topped by a central dome. The temple is decorated with 2,672 relief panels and 504 Buddha statues. The central dome is surrounded by 72 Buddha statues, each seated inside a perforated stupa. It is the world’s largest Buddhist temple, as well as one of the greatest Buddhist monuments in the world.

Built in the 9th century during the reign of the Sailendra Dynasty, the temple was designed in Javanese Buddhist architecture, which blends the Indonesian indigenous cult of ancestor worship and the Buddhist concept of attaining Nirvana. The temple also demonstrates the influences of Gupta art that reflects India's influence on the region, yet there are enough indigenous scenes and elements incorporated to make Borobudur uniquely Indonesian. The monument is both a shrine to the Lord Buddha and a place for Buddhist pilgrimage. The journey for pilgrims begins at the base of the monument and follows a path around the monument and ascends to the top through three levels symbolic of Buddhist cosmology: Kāmadhātu (the world of desire), Rupadhatu (the world of forms) and Arupadhatu (the world of formlessness). The monument guides pilgrims through an extensive system of stairways and corridors with 1,460 narrative relief panels on the walls and the balustrades. Borobudur has the largest and most complete ensemble of Buddhist reliefs in the world.

Evidence suggests Borobudur was constructed in the 9th century and abandoned following the 14th-century decline of Hindu kingdoms in Java and the Javanese conversion to Islam. Worldwide knowledge of its existence was sparked in 1814 by Sir Thomas Stamford Raffles, then the British ruler of Java, who was advised of its location by native Indonesians. Borobudur has since been preserved through several restorations. The largest restoration project was undertaken between 1975 and 1982 by the Indonesian government and UNESCO, following which the monument was listed as a UNESCO World Heritage Site.

Borobudur is still used for pilgrimage; once a year, Buddhists in Indonesia celebrate Vesak at the monument, and Borobudur is Indonesia's single most visited tourist attraction.

Etymology

In Indonesian, ancient temples are referred to as candi; thus locals refer to "Borobudur Temple" as Candi Borobudur. The term candi also loosely describes ancient structures, for example gates and baths. The origins of the name Borobudur, however, are unclear, although the original names of most ancient Indonesian temples are no longer known. The name Borobudur was first written in Sir Thomas Raffles's book on Javan history. Raffles wrote about a monument called Borobudur, but there are no older documents suggesting the same name. The only old Javanese manuscript that hints the monument called Budur as a holy Buddhist sanctuary is Nagarakretagama, written by Mpu Prapanca, a Buddhist scholar of Majapahit court, in 1365.

Most candi are named after a nearby village. If it followed Javanese language conventions and was named after the nearby village of Bore, the monument should have been named "BudurBoro". Raffles thought that Budur might correspond to the modern Javanese word Buda ("ancient")—i.e., "ancient Boro". He also suggested that the name might derive from boro, meaning "great" or "honourable" and Budur for Buddha. However, another archaeologist suggests the second component of the name (Budur) comes from Javanese term bhudhara ("mountain").

Another possible etymology suggests that Borobudur is a corrupted simplified local Javanese pronunciation of Biara Beduhur written in Sanskrit as Vihara Buddha Uhr. The term Buddha-Uhr could mean "the city of Buddhas", while another possible term Beduhur is probably an Old Javanese term, still survived today in Balinese vocabulary, which means "a high place", constructed from the stem word dhuhur or luhur (high). This suggests that Borobudur means vihara of Buddha located on a high place or on a hill.

The construction and inauguration of a sacred Buddhist building—possibly a reference to Borobudur—was mentioned in two inscriptions, both discovered in Kedu, Temanggung Regency. The Karangtengah inscription, dated 824, mentioned a sacred building named Jinalaya (the realm of those who have conquered worldly desire and reached enlightenment), inaugurated by Pramodhawardhani, daughter of Samaratungga. The Tri Tepusan inscription, dated 842, is mentioned in the sima, the (tax-free) lands awarded by Çrī Kahulunnan (Pramodhawardhani) to ensure the funding and maintenance of a Kamūlān called Bhūmisambhāra. Kamūlān is from the word mula, which means "the place of origin", a sacred building to honor the ancestors, probably those of the Sailendras. Casparis suggested that Bhūmi Sambhāra Bhudhāra, which in Sanskrit means "the mountain of combined virtues of the ten stages of Boddhisattvahood", was the original name of Borobudur.

Location
The three temples

Approximately 40 kilometres (25 mi) northwest of Yogyakarta and 86 kilometres (53 mi) west of Surakarta, Borobudur is located in an elevated area between two twin volcanoes, Sundoro-Sumbing and Merbabu-Merapi, and two rivers, the Progo and the Elo. According to local myth, the area known as Kedu Plain is a Javanese "sacred" place and has been dubbed "the garden of Java" due to its high agricultural fertility. During the restoration in the early 20th century, it was discovered that three Buddhist temples in the region, Borobudur, Pawon and Mendut, are positioned along a straight line. A ritual relationship between the three temples must have existed, although the exact ritual process is unknown.

Ancient lake

Speculation about the lake's existence was the subject of intense discussion among archaeologists in the 20th century. In 1931, a Dutch artist and scholar of Hindu and Buddhist architecture, W.O.J. Nieuwenkamp, developed a theory that the Kedu Plain was once a lake and Borobudur initially represented a lotus flower floating on the lake. It has been claimed that Borobudur was built on a bedrock hill, 265 m (869 ft) above sea level and 15 m (49 ft) above the floor of a dried-out paleolake.

Dumarçay together with Professor Thanikaimoni had taken soil samples in 1974 and again in 1977 from trial trenches that had been dug into the hill, as well as from the plain immediately to the south. These samples were later analysed by Professor Thanikaimoni, who examined their pollen and spore content in order to identify the type of vegetation that had grown in the area around the time of Borobudur’s construction. They were unable to discover any pollen or spore samples that were characteristic of any vegetation known to grow in an aquatic environment such as a lake, pond or marsh. The area surrounding Borobudur appears to have been surrounded by agricultural land and palm trees at the time of the monument’s construction, as is still the case today. Caesar Voûte and the geomorphologist Dr J.J. Nossin in 1985–86 field studies re-examined the Borobudur lake hypothesis and concluded the absence of a lake around Borobudur at the time of its construction and active use as a sanctuary. These findings A New Perspective on Some Old Questions Pertaining to Borobudur were published in the 2005 UNESCO publication titled "The Restoration of Borobudur".

History
Construction

There is no written record of who built the Borobudur or of its intended purpose. The construction time has been estimated by comparison between carved reliefs on the temple's hidden foot and the inscriptions commonly used in royal charters during the 8th and 9th centuries. Borobudur was likely founded around 800 CE. This corresponds to the period between 760 and 830 CE, the peak of the Sailendra dynasty rule upon Mataram kingdom in central Java, when it was under the influence of the Srivijayan Empire. The construction has been estimated to have taken 75 years and been completed during the reign of Samaratungga in 825.

There is confusion between Hindu and Buddhist rulers in Java around that time. The Sailendras were known as ardent followers of Buddhism, though stone inscriptions found at Sojomerto suggest they may have been Hindus. It was during this time that many Hindu and Buddhist monuments were built on the plains and mountains around the Kedu Plain. The Buddhist monuments, including Borobudur, were erected around the same period as the Hindu Shiva Prambanan temple compound. In 732 CE, the Shivaite King Sanjaya commissioned a Shivalinga sanctuary to be built on the Wukir hill, only 10 km (6.2 mi) east of Borobudur.

Construction of Buddhist temples, including Borobudur, at that time was possible because Sanjaya's immediate successor, Rakai Panangkaran, granted his permission to the Buddhist followers to build such temples. In fact, to show his respect, Panangkaran gave the village of Kalasan to the Buddhist community, as is written in the Kalasan Charter dated 778 CE. This has led some archaeologists to believe that there was never serious conflict concerning religion in Java as it was possible for a Hindu king to patronize the establishment of a Buddhist monument; or for a Buddhist king to act likewise. However, it is likely that there were two rival royal dynasties in Java at the time—the Buddhist Sailendra and the Saivite Sanjaya—in which the latter triumphed over their rival in the 856 battle on the Ratubaka plateau. This confusion also exists regarding the Lara Jonggrang temple at the Prambanan complex, which was believed to have been erected by the victor Rakai Pikatan as the Sanjaya dynasty's reply to Borobudur, but others suggest that there was a climate of peaceful coexistence where Sailendra involvement exists in Lara Jonggrang.

Abandonment

Borobudur lay hidden for centuries under layers of volcanic ash and jungle growth. The facts behind its abandonment remain a mystery. It is not known when active use of the monument and Buddhist pilgrimage to it ceased. Sometime between 928 and 1006, King Mpu Sindok moved the capital of the Medang Kingdom to the region of East Java after a series of volcanic eruptions; it is not certain whether this influenced the abandonment, but several sources mention this as the most likely period of abandonment. The monument is mentioned vaguely as late as ca. 1365, in Mpu Prapanca's Nagarakretagama, written during the Majapahit era and mentioning "the vihara in Budur". Soekmono (1976) also mentions the popular belief that the temples were disbanded when the population converted to Islam in the 15th century.

The monument was not forgotten completely, though folk stories gradually shifted from its past glory into more superstitious beliefs associated with bad luck and misery. Two old Javanese chronicles (babad) from the 18th century mention cases of bad luck associated with the monument. According to the Babad Tanah Jawi (or the History of Java), the monument was a fatal factor for Mas Dana, a rebel who revolted against Pakubuwono I, the king of Mataram in 1709. It was mentioned that the "Redi Borobudur" hill was besieged and the insurgents were defeated and sentenced to death by the king. In the Babad Mataram (or the History of the Mataram Kingdom), the monument was associated with the misfortune of Prince Monconagoro, the crown prince of the Yogyakarta Sultanate in 1757. In spite of a taboo against visiting the monument, "he took what is written as the knight who was captured in a cage (a statue in one of the perforated stupas)". Upon returning to his palace, he fell ill and died one day later.

Rediscovery

Following its capture, Java was under British administration from 1811 to 1816. The appointed governor was Lieutenant Governor-General Thomas Stamford Raffles, who took great interest in the history of Java. He collected Javanese antiques and made notes through contacts with local inhabitants during his tour throughout the island. On an inspection tour to Semarang in 1814, he was informed about a big monument deep in a jungle near the village of Bumisegoro. He was not able to make the discovery himself and sent H.C. Cornelius, a Dutch engineer, to investigate. In two months, Cornelius and his 200 men cut down trees, burned down vegetation and dug away the earth to reveal the monument. Due to the danger of collapse, he could not unearth all galleries. He reported his findings to Raffles, including various drawings. Although the discovery is only mentioned by a few sentences, Raffles has been credited with the monument's recovery, as one who had brought it to the world's attention.

Hartmann, a Dutch administrator of the Kedu region, continued Cornelius's work, and in 1835, the whole complex was finally unearthed. His interest in Borobudur was more personal than official. Hartmann did not write any reports of his activities, in particular, the alleged story that he discovered the large statue of Buddha in the main stupa. In 1842, Hartmann investigated the main dome, although what he discovered is unknown and the main stupa remains empty.


The Dutch East Indies government then commissioned F.C. Wilsen, a Dutch engineering official, who studied the monument and drew hundreds of relief sketches. J.F.G. Brumund was also appointed to make a detailed study of the monument, which was completed in 1859. The government intended to publish an article based on Brumund's study supplemented by Wilsen's drawings, but Brumund refused to cooperate. The government then commissioned another scholar, C. Leemans, who compiled a monograph based on Brumund's and Wilsen's sources. In 1873, the first monograph of the detailed study of Borobudur was published, followed by its French translation a year later. The first photograph of the monument was taken in 1872 by a Dutch-Flemish engraver, Isidore van Kinsbergen.

Appreciation of the site developed slowly, and it served for some time largely as a source of souvenirs and income for "souvenir hunters" and thieves. In 1882, the chief inspector of cultural artifacts recommended that Borobudur be entirely disassembled with the relocation of reliefs into museums due to the unstable condition of the monument. As a result, the government appointed Groenveldt, an archeologist, to undertake a thorough investigation of the site and to assess the actual condition of the complex; his report found that these fears were unjustified and recommended it be left intact.

Borobudur was considered as the source of souvenirs, and parts of its sculptures were looted, some even with colonial-government consent. In 1896 King Chulalongkorn of Siam visited Java and requested and was allowed to take home eight cartloads of sculptures taken from Borobudur. These includes thirty pieces taken from a number of relief panels, five buddha images, two lions, one gargoyle, several kala motifs from the stairs and gateways, and a guardian statue (dvarapala). Several of these artifacts, most notably the lions, dvarapala, kala, makara and giant waterspouts are now on display in the Java Art room in The National Museum in Bangkok.

Restoration

Borobudur attracted attention in 1885, when Yzerman, the Chairman of the Archaeological Society in Yogyakarta, made a discovery about the hidden foot. Photographs that reveal reliefs on the hidden foot were made in 1890–1891. The discovery led the Dutch East Indies government to take steps to safeguard the monument. In 1900, the government set up a commission consisting of three officials to assess the monument: Brandes, an art historian, Theodoor van Erp, a Dutch army engineer officer, and Van de Kamer, a construction engineer from the Department of Public Works.

In 1902, the commission submitted a threefold plan of proposal to the government. First, the immediate dangers should be avoided by resetting the corners, removing stones that endangered the adjacent parts, strengthening the first balustrades and restoring several niches, archways, stupas and the main dome. Second, after fencing off the courtyards, proper maintenance should be provided and drainage should be improved by restoring floors and spouts. Third, all loose stones should be removed, the monument cleared up to the first balustrades, disfigured stones removed and the main dome restored. The total cost was estimated at that time around 48,800 Dutch guilders.

The restoration then was carried out between 1907 and 1911, using the principles of anastylosis and led by Theodor van Erp. The first seven months of restoration were occupied with excavating the grounds around the monument to find missing Buddha heads and panel stones. Van Erp dismantled and rebuilt the upper three circular platforms and stupas. Along the way, Van Erp discovered more things he could do to improve the monument; he submitted another proposal, which was approved with the additional cost of 34,600 guilders. At first glance, Borobudur had been restored to its old glory. Van Erp went further by carefully reconstructing the chhatra (three-tiered parasol) pinnacle on top of the main stupa. However, he later dismantled the chhatra, citing that there were not enough original stones used in reconstructing the pinnacle, which means that the original design of Borobudur's pinnacle is actually unknown. The dismantled chhatra now is stored in Karmawibhangga Museum, a few hundred meters north from Borobudur.

Due to the limited budget, the restoration had been primarily focused on cleaning the sculptures, and Van Erp did not solve the drainage problem. Within fifteen years, the gallery walls were sagging, and the reliefs showed signs of new cracks and deterioration. Van Erp used concrete from which alkali salts and calcium hydroxide leached and were transported into the rest of the construction. This caused some problems, so that a further thorough renovation was urgently needed.

Small restorations have been performed since then, but not sufficient for complete protection. During World War II and Indonesian National Revolution in 1945 to 1949, Borobudur restoration efforts were halted. The monument suffered further from the weather and drainage problems, which caused the earth core inside the temple to expand, pushing the stone structure and tilting the walls. By 1950s some parts of Borobudur were facing imminent danger of collapsing. In 1965, Indonesia asked the UNESCO for advice on ways to counteract the problem of weathering at Borobudur and other monuments. In 1968 Professor Soekmono, then head of the Archeological Service of Indonesia, launched his "Save Borobudur" campaign, in an effort to organize a massive restoration project.

In the late 1960s, the Indonesian government had requested from the international community a major renovation to protect the monument. In 1973, a master plan to restore Borobudur was created. The Indonesian government and UNESCO then undertook the complete overhaul of the monument in a big restoration project between 1975 and 1982. In 1975, the actual work began. Over one million stones were dismantled and removed during the restoration, and set aside like pieces of a massive jig-saw puzzle to be individually identified, catalogued, cleaned and treated for preservation. Borobudur became a testing ground for new conservation techniques, including new procedures to battle the microorganisms attacking the stone. The foundation was stabilized, and all 1,460 panels were cleaned. The restoration involved the dismantling of the five square platforms and the improvement of drainage by embedding water channels into the monument. Both impermeable and filter layers were added. This colossal project involved around 600 people to restore the monument and cost a total of US$6,901,243.

After the renovation was finished, UNESCO listed Borobudur as a World Heritage Site in 1991. It is listed under Cultural criteria (i) "to represent a masterpiece of human creative genius", (ii) "to exhibit an important interchange of human values, over a span of time or within a cultural area of the world, on developments in architecture or technology, monumental arts, town-planning or landscape design", and (vi) "to be directly or tangibly associated with events or living traditions, with ideas, or with beliefs, with artistic and literary works of outstanding universal significance".

Trio Gili Island


The islands are a popular destination for tourists looking for a remote island experience. Each island has several small resorts, usually consisting of a collection of huts for tourists, a small pool and restaurant. Most local inhabitants live on Trawangan in a township stretching along its east side just inland (which is also where most recent development is taking place). Automobiles and motorised traffic is prohibited on the islands by local ordinance, so the preferred method of transportation is by foot and bicycle or the horse-drawn carriage called a cidomo. Diving in and around the Gilis is also popular due to the abundance of marine life and attractive coral formations.

Etymology

The name "Gili Islands" is a misnomer, because Gili simply means "small island" in Sasak. As a result, most of the islands around the coast of Lombok have Gili in their names, although confusion is averted by referring (in English) to the other Gilis around the Lombok coast by their proper names only.

The Indonesian word for water is Air (AH-yer) and Gili Air was named for the being the only island of the three to have subterranean fresh water. This is acknowledged as a finite resource with some resorts and restaurants shipping in the water from the mainland.

Geography and climate

The Islands are located in the Lombok Strait, to the immediate northwest of Lombok. They extend outward from a tiny peninsula called Sire near to the village of Tanjung on Lombok. Bali lies about 35 km to the west of Gili Trawangan, the islands' most westerly member. Both Bali and Lombok are easily visible from the Gilis in clear weather. Mount Rinjani, Indonesia's second highest volcano, is close by on neighbouring Lombok, and dominates the views towards the east.

Due to their close proximity to the Equator, the Islands have a warm, Tropical climate with a dry and wet season. With Mount Rinjani to the immediate east on Lombok, and Mount Agung to the west on Bali, The Gilis are somewhat sheltered and actually enjoy a slightly drier Microclimate when compared to the surrounding archipelago. Dry Season usually last from May until October, with Monsoon season starting in November and continuing through to April. Temperatures range between 22 °C to 34 °C, with an average annual temperature of around 28 °C.

Demography

Although specific census records for the Gili Islands alone are not available (being incorporated into the regional census), according to the annual written register of "Kepala Desa Gili Indah" (head of the 3 Gili Islands), Mr. H.Taufiq, Gili Air has 450 families, Gili Meno 172, and Gili Trawangan 361. This puts the number of registered resident Indonesian families on the islands at 983 as of 2012.

The significant number of permanent western residents is difficult to quantify as there are no official statistics to date.

History

Due to the small size, population and relatively recent settlement of the Islands, published sources are limited. Where local knowledge has been used, those cited are elected local officials whose details are listed in the references section. For more detailed regional historical information, visit the Lombok article.

For a brief period during the second world war, occupying Japanese forces used the islands as a lookout post and prisoner of war camp. Relics from this period include the remains of a bunker on the hill of Gili Trawangan and the wreck of a patrol boat submerged at a depth of 45 m in the bay to the south of Gili Air (now a popular dive site). Permanent settlement only began in the 1970s, mainly due to the lack of fresh water sources before that time. Previous to human settlement, these islands remained pristine wildlife mangrove habitats.

Initially, Bugis fishermen used the islands as a stop off location for their voyages around the archipelago. In 1971 the governor of Lombok, Wasita Kusama, began to establish coconut plantations and gave land rights to private companies. 350 inmates from overcrowded Mataram prison were sent to help with the first harvests between 1974 and 1979, many of whom remained on the Islands as permanent settlers. Following various difficulties with coconut harvests, the private efforts to exploit the islands' plantations were abandoned. The local population grew beyond their allocated bounds (100 hectares) and began to erect homes and businesses on the private, abandoned land. This led to a land dispute that continues to the present.

In the 1980s, the islands started to be discovered by backpacker tourists. This was influenced by the exponential rise of tourism in neighbouring Bali. At first, Gili Air (having the most infrastructure at the time) began to transform to cater to this new economy, however, Gili Trawangan soon surpassed it due mostly to its proximity to better dive locations.

As the prospects for tourism on the islands began to rise in the late 1980s and early 1990s, the government and investors whose abandoned land had been settled on by an expanding population, began to regain interest in the potential for development. This resulted in a series of evictions and demolishing of local homes and businesses, followed each time by no action on the part of the developers and a rebuilding of destroyed homes by residents who opposed the eviction.

The first tourist accommodation on Gili Trawangan was a small homestay called Pak Majid, built in 1982, by Pak ("polite Mr") Majid. This was eventually taken over in 2007 and transformed into Pesona Resort and Restaurant (the first Indian restaurant on the Gilis). Most of the locally owned businesses from the 1980s have been acquired by westerners. The longest standing locally owned and operated business is "Goodheart" resort, originally built in 1987 and rebuilt three times following demolition relating to the ongoing land dispute.

Gili Trawangan gained a reputation from the late 1980s to the late 1990s as a party island. Drugs were freely available on the island and its low population and remoteness required no police presence at the time.

During the 1990s, the Diving industry grew swiftly and the Islands began to develop into a world class diving instruction location. This fed local tourism and in the new millennium a wider spectrum of accommodation and entertainment began to be developed that catered to a broader range of visitors.

In 2000, a non-profit organisation by the name of Gili Eco Trust was established to help protect the coral reefs surrounding the islands and improve environmental education. It originated as a co-operation between influential members of the local community (Satgas) and the dive shops on Gili Trawangan and was initiated by the owners of Manta Dive. Many projects have since been organised to protect and restore coral reefs, improve waste management, struggle against erosion, treat animals, raise awareness and educate. This was needed as damage had occurred due to a particularly warm El Niño and unsustainable local fishing methods.

In 2005, fast boat operations began from neighbouring Bali, the first company being Blue Water Express, they still operate to the islands. Following them, fast boat services from several operators commenced services from various points around Bali and Nusa Lembongan, to the Islands.

As of 2012, The islands continue to experience rapid growth and development related to the tourism industry. Efforts are being made to preserve marine habitats and remain culturally distinct from neighbouring Bali in this process. The aforementioned land dispute remains unresolved.

Gili Trawangan

Gili Trawangan is the largest of Lombok's Gili Islands and the only one to rise significantly (30 m) above sea level. Measuring 3 km long and 2 km wide, it has a population of around 1500 (see demography). The name Trawangan originates from the Indonesian word Terowongan (Tunnel) due to the presence of a cave tunnel built there during Japanese occupation in World War 2. Of the Gilis, Trawangan is the most developed and geared towards tourism. The main concentration of settlement, recreation, accommodation and diving business is situated on the eastern side of the island. A local pub, Tîr na Nôg claims that Trawangan is the smallest island in the world with an Irish pub. It was previously administered under Lombok Barat Regency along with Senggigi until 2010 when the Gili islands came under the jurisdiction of the new North Lombok Regency (Kabupaten Lombok Utara).

On Gili Trawangan (as well as the other two Gilis), there are no motorised vehicles. The main means of transportation are bicycles (rented by locals to tourists) and cidomo (a small horse-drawn carriage). For travelling to and from each of the Gilis, locals usually use motorised boats and speedboats.

Some of the first inhabitants of Gili Trawangan were fishermen and farmers from Sulawesi. Previous to human settlement Gili Trawangan was covered in forest and deer lived on the island.

The economy of Gili Trawangan centres on tourism, as the island is too small to support any broad scale agriculture, and too remote to allow economically viable industry or commerce. There is a mosque on the island.

Drug tourism

Gili Trawangan has had a reputation since the 1980s as a location where drugs are freely available. Psilocybin mushrooms are openly advertised on the island, and a range of harder drugs have been known to be in circulation. Though police presence is low, Indonesian drug laws are extremely harsh and thus strictly speaking drug possession and use is prohibited and carries potentially grave risk (up to and including the death penalty).

In recent years, locally made spirits have caused casualties and even some fatalities among tourists and locals, due to methanol poisoning. Methanol is sometimes used by locals as a cheap way of topping up their stock. The most recent case of this was on New Year's Eve 2012, where a young man was served a cocktail at Rudy's bar that had been infused with methanol. Following misdiagnoses in Indonesia and repatriation, he died 5 days later.

Gili Meno

Gili Meno is the middle of Lombok's three northwest coast Gilis. Gili Meno has a population of about 500, mainly concentrated on the centre of the island (see section on demography). The main income comes from tourism, coconut plantation and fishing. On the west side of the island there is a small shallow lake that produces salt in the dry season. Until a few years ago there was also a small production of seaweed on the reef at the north end of the island. Gili Meno has swimming beaches all around the island, and a turtle sanctuary.

The island attracts fewer tourists than Gili Trawangan and is the quietest and smallest of the islands. However, honeymooners are often drawn to the crystal clear water and idyllic, secluded white beaches.

There is no fresh water on the island and it has to be brought by boat from Lombok. Electricity is supplied by underwater cables from Lombok. There are no cars or motorbikes.

Gili Air

Gili Air is the second smallest of the islands and the closest to mainland Lombok, making it popular with honeymoon couples and travellers seeking a quiet retreat. It has a population of about 1,800. The island offers excellent snorkelling and scuba diving off its east coast, and turtles can be seen along the coral reef. Other water sports such as Stand Up Paddleboarding and Kitesurfing are also now available.

Continued investment in tourism is seeing these islands develop very quickly and each year sees new resorts and accommodation on the islands while attempting to retain their individual character. Proximity to Gili Meno, the smallest and most secluded of the islands and to Gili Trawangan the largest island, known for its many restaurants and parties, makes Gili Air a happy Medium of seclusion with adequate services. Both other Islands are a quick boat ride away.

Transport

There is no motorised transport on the Islands. The short distances on land are traversed on foot, by bicycle or Cidomo. The Islands can only be reached by sea, and are frequented by a variety of fast boats operating various routes from Bali.

Flights from Ngurah Rai International Airport (IATA: DPS) to Lombok International Airport (IATA: LOP) take about 40 minutes followed by a 2hr taxi ride to Bangsal harbour in Northwest Lombok and a Local boat to the Gili Islands for a further 20-30mins.

Public Ferries depart from Padang Bai (Southeast Bali) every hour, taking a minimum of 4–5 hours to reach Lembar (Southwest Lombok), after which a taxi can be taken for a 2hr drive to Bangsal harbour where local boats to the Gili Islands await during daylight hours.

There are now numerous direct Fast boat services from Bali to the Gili Islands, all of which also service Lombok, and a few of which pass by Nusa Lembongan en route. Prices and standards vary widely both online and locally, depending on departure point, level of comfort and operating expertise. Established daily services depart from Benoa and Serangan in South Bali and from Padangbai and Amed (Bali) in East and Northeast Bali respectively. Benoa Harbour and Serangan are around 25 min by car, (dependent upon traffic) from Kuta and the main South Bali tourist hub. Padang Bai is about another hour by road from the same point of reference. In 2011, the Gilibookings website made first provision for online e-ticketing for the fast boat sector.


Tana Toraja Regency


Tana Toraja Regency (Torajaland, Land of the Toraja or Tator) is a regency (kabupaten) of South Sulawesi Province of Indonesia, and home to the Toraja ethnic group. The local government seat is in Makale, while the center of Toraja culture is in Rantepao. But now, Tana Toraja has been divided to two regencies that consist of Tana Toraja with its capital at Makale and Toraja Utara with its capital at Rantepao.

The Tana Toraja boundary was determined by the Dutch East Indies government in 1909. In 1926, Tana Toraja was under the administration of Bugis state, Luwu. The regentschap (or regency) status was given on 8 October 1946, the last regency given by the Dutch. Since 1984, Tana Toraja has been named as the second tourist destination after Bali by the Ministry of Tourism, Indonesia. Since then, hundreds of thousands of foreign visitors have visited this regency. In addition, numerous Western anthropologists have come to Tana Toraja to study the indigenous culture and people of Toraja.

Attractions

Tana Toraja is one of the major tourist attraction Indonesia, inhabited by the Toraja people who live in mountainous areas and maintain a lifestyle that was typical and lifestyle shows Austronesian origins and cultures similar to Nias. This area is one of the attractions in South Sulawesi.

Appendicitis Kalando
Tongkonan / house money Sangalla '(King Sangalla') silence. As a resting place Sangala money 'and is also a palace where the royal government to manage Sangalla' at that time, Tongkonan Dead Kalando called "reservoir Langi detainees' loud Kaero tongkonan Layuk". Appendicitis is currently Tongkonan Kalando made Museum Place store objects and relics of prehistoric empire Sangalla '.

Pallawa
Tongkonan alphabet is one tongkonan or custom homes are very attractive and are among the bamboo trees on a hilltop. Tongkonan is decorated with a buffalo horn stuck on the front of the house. Located about 12 km north of Independence.

Londa
Londa is a steep rock on the side of the tomb is typical of Tana Toraja. One of them is located in a high place of a hill with a cave in which the coffins the bodies set up in accordance with the family, in the other side of the hill overlooking left open expanse of green. Located about 5 km south of Independence.

Kete Kesu
Object charming village in the form of Tongkonan, barns and buildings in the surrounding megaliths. Approximately 100 meters behind the village there are cliffs with burial sites and grave dependent tau-tau in a stone building that fence. Tau-tau appearance owner daily. The village is also known by the membership sculptures owned by its residents as well as a great place to shop for souvenirs. Located about 4 km southeast of Padang.

Stone Tumonga
In this area you can find around 56 stone menhirs in a circle with 4 trees in the middle. Most stone menhirs have a height of about 2-3 meters. From here you can see the beauty of the surrounding valley and parades. Located in an area with a height of Sesean 1300 meters above sea level.

Lemo
It is often referred to as the home of the spirits. At the funeral Lemo we can see a dead body that sets stored in the open air, in the middle of a steep rock. This cemetery is a blend of death, art and ritual. At certain times of the clothes the corpses will be replaced with a ceremony Ma 'Nene.

Conservation efforts
Tana Toraja is one of the conservation of cultural civilization Proto-Malays Austronesian preserved until now. Cultural traditions, music, dance, oral literature, language, home, carving, weaving and culinary still very traditional, making the Indonesian Government to strive for Tana Toraja can be known in the international world, one of which is to nominate Tana Toraja to UNESCO for a UNESCO World Heritage Site since 2009.

This is supported by the Japanese to make Tana Toraja as UNESCO World Heritage Site, Japan itself will participate in conservation efforts, particularly associated with traditional houses in the area.

Support is delivered in a meeting between the delegations of Indonesia and Japan in Poznan, Poland, on Saturday (11/9/2010), The meeting was held after the pilot Ministerial Meeting on Culture of Asia and Europe (Asia-Europe Culture Ministers Meeting / ASEM), the fourth to 9- 10 September in Poznan, which was attended by representatives of about 40 countries in Asia and Europe

Jayawijaya Mountains


Puncak Jaya is a summit that is part of the Sudirman Range found in Papua Province, Indonesia. Puncak Jaya has an altitude of 4884 m and in the vicinity there Carstensz glacier, the only glacier in tropical Indonesia, which likely will soon vanish due to global warming.

This peak is the highest mountain in Indonesia Oceania region. Puncak Jaya is one of the world's top seven.

History
Discovery

The plateau around the summit originally was inhabited before any contact with Europeans, and the peak known as Nemangkawi in Amungkala. Puncak Jaya, formerly named Carstensz Pyramid after Dutch explorer Jan Carstenszoon called it when I first saw the glacier at the summit of the mountain on a sunny day in 1623.

Snowfield (glacier) Puncak Jaya managed to climb in early 1909 by a Dutch explorer, Hendrikus Albertus Lorentz with six Kenyah recruited from Apau Kayan in North Borneo. Lorentz National Park, which also includes the Carstensz Pyramid, established in 1919 following a report of this expedition.

Climbing History

In 1936, an expedition to Carstensz initiated by the Dutch, unable to establish with certainty which of the three is the highest peak, decided to try to climb each peak. Anton Colijn, Jean Jacques Dozy and Frits Julius Wissel reached Carstensz glacier field and East Peak Guns Pulu on 5 December. As glaciers melt, the height of the peak of the 4,862 Guns Pulu meters, but it has been estimated that in 1936 (when glaciers still covered peak of 13 square kilometers), Guns Pulu is the highest peak with an altitude of over 5,000 meters.

Afterwards Puncak Jaya never climbed until 1962, by an expedition led by the Austrian mountaineer Heinrich Harrer, with three other members of the expedition, Robert Philip Temple, Russell Kippax, and Albert Huizenga. Philip Temple of New Zealand, previously led an expedition to the region and pave the access routes to the mountain.

In 1963, the peak was renamed Peak International, after it was changed to Puncak Jaya. Name of the Carstensz Pyramid is still used among mountaineers.

Glacier

Meanwhile, Puncak Jaya is still a little icy, there are several glaciers on the slopes, including the Carstensz Glacier, Glacier Northwall Firn West, and East Glacier Northwall Firn, recently rumored to vanish.

Glaciers in Puncak Trikora Maoke disappear altogether in the period between 1939 and 1962. Since 1970, evidence from satellite imagery shows Puncak Jaya glaciers have been shrinking rapidly. Meren Glacier melt between 1994 and 2000. An expedition led by paleoclimatologist Lonnie Thompson in 2010 found that the glaciers are disappearing at a rate of 7 meters in thickness per year and will disappear completely in 2015.

Sentani Lake


Lake Sentani is a tropical, shallow, and at low-altitude open lake located at the northeast extremity of the Intan Jaya Regency in the Indonesian province of Papua, about 20 kilometres (12 mi) from the provincial capital, Jayapura City.

The lake, which is considered by the local population as the home of the rainbows, is part of the Cyclops Strict Nature Reserve and contains many species of fish that cannot be found anywhere else in the world.

Hydrology

Lake Sentani lies at the foot of the Mesozoic mafic and ultramafic rocks of the Cyclops ophiolite mountains in a fault-controlled depression at an elevation of 73 metres (240 ft) above the level of the sea. Sentani is an irregularly shaped body with approximate maximum length extending from east to west of 28 kilometres (17 mi) and, from north to south, 19 kilometres (12 mi) of breadth. With a surface area of 104 square kilometres (40 sq mi), Lake Sentani is the largest lake of the Intan Jaya region.

Lake Sentani receives its water primarily from direct precipitation with an average annual rainfall around the lake of about 2 metres (6.6 ft), and by mountain streams. The average evaporation on the lake is about 0.4 metres (1.3 ft) with seasonal variation in inflow. The lake outflows into the Jafuri and Tami rivers to the Pacific Ocean near the Papua New Guinea border.

Geology

Lake Sentani, the best studied of Irian Jaya lakes, is relatively stable and intact. It is widely believed to have evolved by the tectonic damming and uplift of an arm of the sea, but such a connection has not been demonstrated yet.

Natural history

Lake Sentani is thermally stable, with temperatures ranging from 29 to 32 °C (84 to 90 °F) in the top 10 metres (33 ft); the surface pH is 6.2–6.8, and plankton levels are low at 1–2 mg/L except in the westernmost basin, where water circulation is limited, turbidity is doubled, and seasonal algal blooms, with resultant fish mortality. Preliminary bottom sediment samples from the eastern part of the lake have yielded sparse populations of arcellacean microfauna, dominated by Centropyxid types. In other parts of the world these species are found associated with brackish or polluted water conditions, raising the possibility that there is residual salinity in the deeper parts of the lake.

It may be small, but it harbors 33 species of fish, of which 12 are indigenous, 8 anadromous and 13 introduced. Besides having its own species of rainbowfish (Sentani rainbowfish and red rainbowfish), Lake Sentani is also home to another fish species that cannot be found anywhere else, the Sentani gudgeon. Sawfish up to 3 metres (9.8 ft) were well known in the lake until the 1970s and are a common motif in traditional Sentani art, but appear to have become extinct. Fish are extensively raised in ponds and cages around the perimeter of the lake and the introduction of species (particularly carp and tilapia) has been both accidental and intentional.

In this part of the world and at this latitude rainbows are visible only after a hard rain, but in Lake Sentani they are visible all the time, at least, by seeing the Sentani rainbowfish that, along with many others, are unique to this lake.

Economy

Many of the Sentani people, who inhabit the islands, perimeter and environs of the lake, still have a traditional subsistence economy based on fishing and sago harvesting. This has been sustainable for centuries but local reports suggest that catch yields have diminished in recent years. Whether this is a result of overfishing (as a result of population growth and/or market pressure), pollution or introduction of foreign species is not established. Many of the residents occupy dwellings built on posts over the lake, which thus serves as a depository for sewage, leading to locally high coliform bacteria counts, but also to nutrient enrichment. Water hyacinth (Eichornia crassipes), introduced since the early 1970s, has become a major plant pest and may contribute to the decline of some species.

Much of the mountainous terrain between the north shore of the lake and the ocean falls within the Cyclops Strict Nature Reserve. The future management of the reserve and buffer zone, and the environmental quality of the lake, are strongly interdependent. Recently a major reforestation project of grassland on the slopes surrounding the lake has been initiated, with the support of forest companies operating in Papua. This ecoregion is located within one of the most populated areas of Papua, but it is threatened by overfishing, the introduction of new species, which could be harmful to the endemic species in this lake and aquaculture. A major sustainable development issues for the inhabitants of the lake and surroundings is the existing proposal to build a hydroelectric power plant through a dam placed on the Jafuri river. Several feasibility and environmental impact studies have been published, but the cost/benefit consequences of this project have not been released yet.

Raja Ampat Islands


Located off the northwest tip of Bird's Head Peninsula on the island of New Guinea, in Indonesia's West Papua province, Raja Ampat, or the Four Kings, is an archipelago comprising over 1,500 small islands, cays, and shoals surrounding the four main islands of Misool, Salawati, Batanta, and Waigeo, and the smaller island of Kofiau.

Raja Ampat Regency is a new regency which separated from Sorong Regency in 2004. It encompasses more than 40,000 km² of land and sea, which also contains Cenderawasih Bay, the largest marine national park in Indonesia. It is a part of the newly named West Papua province of Indonesia which was formerly Irian Jaya. Some of the islands are the most northern pieces of land in the Australian continent.

History

The name of Raja Ampat comes from local mythology that tells about a woman who finds seven eggs. Four of the seven eggs hatch and become kings that occupy four of Raja Ampat biggest islands whilst the other three become a ghost, a woman, and a stone.

History shows that Raja Ampat was once a part of Sultanate of Tidore, an influential kingdom from Maluku. Yet, after the Dutch invaded Maluku, it was shortly claimed by the Netherlands.

The first recorded sighting and landing by Europeans of the Ampat Islands was in the person of the Portuguese navigator Jorge de Menezes and his crew in 1526, on route from Biak, the Bird's Head Peninsula, and Waigeo, to Halmahera (Ternate).

The English explorer William Dampier gave his name to Dampier Strait, which separates Batanta island from Waigeo island. To the east, there is a strait that separates Batanta from Salawati. In 1759 Captain William Wilson sailing in the East Indiaman Pitt navigated these waters and named one strait Pitt strait, after his vessel; this was probably the channel between Batanta and Salawati.

Population

The main occupation for people around this area is fishing since the area is dominated by the sea. They live in a small colony of tribes that spreads around the area. Although traditional culture still strongly exists, they are very welcoming to visitors. Raja Ampat people are more like Ambonese than Papuan people and now some of them are Muslim and some of them are Christian.

Geography

The oceanic natural resources around Raja Ampat give it significant potential as a tourist area. Many sources place Raja Ampat as one of their top ten most popular places for diving whilst it retains the number one ranking in terms of underwater biodiversity.

According to Conservation International, marine surveys suggest that the marine life diversity in the Raja Ampat area is the highest recorded on Earth. Diversity is considerably greater than any other area sampled in the Coral Triangle composed of Indonesia, Malaysia, Philippines, Papua New Guinea, Solomon Islands, and East Timor. The Coral Triangle is the heart of the world's coral reef biodiversity, making Raja Ampat quite possibly the richest coral reef ecosystems in the world.

The area's massive coral colonies along with relatively high sea surface temperatures, also suggest that its reefs may be relatively resistant to threats like coral bleaching and coral disease, which now jeopardize the survival of other coral ecosystems around the world. The Raja Ampat islands are remote and relatively undisturbed by humans.

The high marine diversity in Raja Ampat is strongly influenced by its position between the Indian and Pacific Oceans, as coral and fish larvae are more easily shared between the two oceans. Raja Ampat's coral diversity, resilience, and role as a source for larval dispersal make it a global priority for marine protection.

1,508 fish species, 537 coral species (a remarkable 96% of all scleractinia recorded from Indonesia are likely to occur in these islands and 75% of all species that exist in the world), and 699 mollusk species, the variety of marine life is staggering. Some areas boast enormous schools of fish and regular sightings of sharks, such as wobbegongs.

Raja Ampat Islands have at least three ponds containt unpoisoned jellyfish, all in Misool area.

Although accessing the islands is not that difficult, it takes some time. It takes six hours flight from Jakarta, the capital city of Indonesia to Sorong. Then, taking a boat to reach the islands is necessary.

Documentary film

The documentary film Edies Paradies 3 (by Otto C. Honegger) has been broadcast by the biggest Switzerland television broadcaster, Schweizer Fernsehen. The film tells about Raja Ampat's natural underwater beauty which is likened to Switzerland's only inhabited area of the region of around 50,000 residents and is considered like the "Amazon" because of the underwater world located in the heart of the world's Coral Triangle.

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