Showing posts with label Mount. Show all posts
Showing posts with label Mount. Show all posts

Tuesday, September 21, 2010

Puncak Jaya (Carstensz Pyramid)

Puncak Jaya, sometimes called Mount Carstensz or the Carstensz Pyramid, is a mountain in the Sudirman Range, the western central highlands of Papua province, Indonesia. Other names include Nemangkawi in the Amungkal language, Ngga Pulu, Carstensz Toppen and Gunung Sukarno.
At 4,884 metres (16,024 ft) above sea level, Puncak Jaya is the highest mountain in Indonesia, the highest on the island of New Guinea (which comprises the Indonesian Papua provinces plus Papua New Guinea), the highest of Oceania (Australia), and the 5th highest mountain in political Southeast Asia. It is also the highest point between the Himalayas and the Andes, and the highest island peak in the world. Some sources claim Mount Wilhelm, 4,509 m (14,793 ft), as the highest mountain peak in Oceania, on account of Indonesia being part of Asia (Southeast Asia).

History


The highlands surrounding the peak were inhabited before European contact, and the peak was known as Nemangkawi in Amungkal. Puncak Jaya was named "Carstensz Pyramid" after Dutch explorer Jan Carstensz who first sighted the glaciers on the peak of the mountain on a rare clear day in 1623. The sighting went unverified for over two centuries, and Carstensz was ridiculed in Europe when he said he had seen snow near the equator. This name is still used among mountaineers. Although the snowfield of Puncak Jaya was reached as early as 1909 by a Dutch explorer, Hendrik Albert Lorentz with six of his indigenous Dayak Kenyah porters recruited from the Apo Kayan in Borneo, the peak was not climbed until 1962, by an expedition led by the Austrian mountaineer Heinrich Harrer (of Seven Years in Tibet fame) with three friends — Temple, Kippax and Huizenga.

When Indonesia took control of the province in the 1960s, the peak was renamed 'Puntjak Soekarno' (Simplified Indonesian: Puncak Sukarno) or Sukarno Peak, after the first President of Indonesia, later this was changed to Puncak Jaya. Puncak means peak or mountain and Jaya means 'victory', 'victorious' or 'glorious'.

Climbing
The highland area in 2005, with the Grasberg copper mine pit in the foreground. Its summit is at the far end of the central rib.
Puncak Jaya is one of the more demanding climbs in one version of the Seven Summits peak-bagging list. (It is replaced by Mount Kosciuszko in the other version.) It is held to have the highest technical rating, though not the greatest physical demands of that list's ascents. The standard route is up the north face and along the summit ridge, which is all hard rock surface. Despite the large mine, the area is highly inaccessible to hikers and the general public, requiring a 100-km hike from the nearest town with an airport, Timika, to the base camp, which usually takes about four or five days each way.

The mount usually climbed by professional climbers, it needs  complete equipment and the local potter. The route is: Tembagapura or Illaga – Lembah Danau – Danau – Cartetz Peak.


Puncak Jaya Picture

Alternate Name(s) :
Carstensz
Latitude/Longitude (WGS84) :
4° 5' S; 137° 9' E
-4.076859, 137.156262 (Dec Deg)
739391E 9549057N Zone 53 (UTM)
Country :
Indonesia (Highest Point)
State/Province :
Irian Jaya (Highest Point)
Drainage Basins :
Mamberamo
Pacific Ocean
Island :
New Guinea (Highest Point)
Ownership :
Land : Gunung Lorentz
Prominence :
Clean Prominence: 4884 m/16,024 ft
Optimistic Prominence: 4884 m/16,024 ft
Key Col : Ocean 0 m/0 ft
Isolation :
Distance to Higher Peak: 5262.57 km/3270.71 mi
Nearest Higher Neighbor: Yulongxue Shan (NW)

Mount Kerinci

Mount Kerinci (also spelled Kerintji, among several other ways, and referred to as Gunung Kerinci, Gadang, Berapi Kurinci, Kerinchi, Korinci, or Peak of Indrapura as well) is the highest volcano in Indonesia, and the highest peak in Sumatra. It is surrounded by the lush forest of Kerinci Seblat National Park, home to the endangered species of sumatran tiger and sumatran rhinoceros.


Location
It is located in Province of Jambi, the west central part of the island, in the Pegunungan/Bukit Barisan, near the west coast, and is about 130 km (81 mi) south of Padang. It is the most prominent feature of the terrain of Kerinci Seblat National Park, with pine-forested slopes rising 2,400-3,300 metres above the surrounding basin, and a cone 13 km (8 mi) wide and 25 km (16 mi) long at the base, elongated in the north-south direction. At the summit there is a deep 600 m (1,969 ft) wide crater, often partially filled with green-yellow water.

Kerinci is more active than most Indonesian volcanoes, with nearly annual phreatic eruptions. Kerinci last erupted in 2004, and continues to spew clouds of sulphurous smoke, with plumes reaching as high as 1,000 m (3,281 ft) above the summit. While there is farmland in the area, and a tea plantation on its southern slope, Kerinci, being located in an Indonesian national park, and perhaps out of respect for its frequent growlings as well, sits in an area that is sparsely populated by Indonesian population-density standards.

Kerinci can be climbed from the village of Kersik Tuo, 6 or 7 hours away from Padang by car or bus. The climb and descent normally takes 3 days and 2 nights, if you choose to go to the summit. You may also choose to go up only till Camp 2 or 2.5, skipping the summit attempt which is a night climb; and take 2 days and 1 night instead.
As of November 2007, the alert level for Kerinci was raised to Level 2- Orange, due to black smog seen coming out of the crater. But climbing the volcano is still relatively safe and allowed; though you may not climb any further than 1 km to the crater.

Kerinci's terrain consists of thick jungle, it can get muddy and slippery even if there are only mild drizzles, which may occur occasionally even during the dry season. To climb the volcano you need a guide, for there have been rare cases of people disappearing after attempting to trek alone.

Climbing
If you want to reach the peak you can take this track: [Bangko – Sungai penuh - Kersik Tuo (tugu macan)] – R Sepuluh – Pintu Rimbo – Pesanggrahan I – Pesanggrahan II – Pesanggrahan III/ POS I (Base camp I) – POS II (Base camp II) – POS III (Base camp III) – The Peak of Mount Kerinci
From the peak, you can see exotic landscape, and the horizon of Hindia Ocean on the west direction.

  Mount Kerinci Picture


Country: Indonesia 
Subregion Name: Sumatra (Indonesia) 
Volcano Number: 0601-17= 
Volcano Type: Stratovolcano 
Volcano Status: Historical 
Last Known Eruption: 2008 
Summit Elevation: 3800 m 12,467 feet
Latitude: 1.697°S 1°41'50"S 
Longitude: 101.264°E 101°15'52"E

Mount Merapi

Mount Merapi, Gunung Merapi, is a conical volcano located on the border between Central Java and Yogyakarta, Indonesia. It is the most active volcano in Indonesia and has erupted regularly since 1548. It is very close to the city of Yogyakarta, and thousands of people live on the flanks of the volcano, with villages as high as 1700 m above sea level.

Although smoke can be seen emerging from the mountain top at least 300 days a year, several eruptions have caused fatalities. Hot gas from a large explosion killed 64 people on November 22 in 1994, mostly in the town of Muntilan, west of the volcano. Another large eruption occurred in 2006, shortly before the Yogyakarta earthquake. In light of the hazards that Merapi poses to populated areas, it has been designated as one of the Decade Volcanoes.

Merapi is the youngest in a group of volcanoes in southern Java. It is situated at a subduction zone, where the Indo-Australian Plate is sliding beneath the Eurasian Plate. It is one of at least 129 active volcanoes in Indonesia, part of the Pacific Ring of Fire – a section of fault lines stretching from the Western Hemisphere through Japan and South East Asia. Stratigraphic analysis reveals that eruptions in the Merapi area began about 400,000 years ago, and from then until about 10,073 years ago, eruptions were typically effusive, and the outflowing lava emitted was basaltic. Since then, eruptions have become more explosive, with viscous andesitic lavas often generating lava domes. Dome collapse has often generated pyroclastic flows, and larger explosions, which have resulted in eruption columns, have also generated pyroclastic flows through column collapse.

Climbing
You can access the highest peak, named Garuda Peak, passing 3 route:

Track I (north track) : [Surakarta – Boyolali – Selo] – Lencoh – Watu Pecah – Pasar Bubrah - Merapi Peak.

Track II (South track) : [Jogja – Kaliurang – Kinahrejo] – Kendit – Merapi Peak.

Track III (West track) : [Yogyakarta – Muntilan – Babadan] – Klatakan – Merapi Peak.

 Mount Merapi Picture

Country: Indonesia 
Subregion Name: Java (Indonesia) 
Volcano Number: 0603-25= 

Volcano Type: Stratovolcano
Volcano Status: Historical 
Last Known Eruption: 2008 
Summit Elevation: 2968 m 9,737 feet 
Latitude: 7.542°S 7°32'30"S 
Longitude: 110.442°E 110°26'30"E

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 (NTB). It rises to 3,726 metres (12,224 ft), making it the second highest volcano in Indonesia, and similar in height to Mount Fuji, the third highest mountain of the Indonesian archipelago and the thirty ninth most prominent peak in the world.
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 (G.Baru). 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.
The 6 km by 8.5 km oval-shaped caldera is filled partially by the crater lake known as Segara Anak ('Child of the Sea') This lake is approximately 2000 metres above sea level and estimated at being around 200 metres deep; the caldera also contains hot springs.
The Rinjani caldera forming eruption is thought to have occurred in the 13th century. Eruption rate, eruption sites, eruptiion 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 2300 metres 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 Mount Barujari (or 'New Finger Mountain').
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.
The volcano and the caldera are protected by the Gunung Rinjani National Park established in 1997. Tourism is increasingly popular with trekkers able to visit the rim, make their way into the caldera or even to make the more arduous climb to the highest point; fatalities, however, are not uncommon. In July 2009 the summit route was closed due to volcanic activity at that time and subsequently reopened when the activity decreased. During early 2010 up to and including May 2010 access to Rinjani was at times again restricted due to volcanic activity.
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 km from the eruption at Gunung Barujari.

Rinjani National park
Gunung Rinjani National Park (Taman Nasional Gunung Rinjani) is popular for mountain climbs and trekking and represents an important nature reserve and water catchement area. The park is officially 41,330 hectares within the park boundaries and includes a further 66,000 hectares of protected forest outside. The mountain and its satellites form the Mount Rinjani National Park (Taman Nasional Gunung Rinjani) - officially 41,000 hectares within the park boundaries and a further 66,000 hectares of protected forest outside. In 2008, the Indonesian government proposed to UNESCO that Mount Rinjani be one of the world's official geoparks. If this was approved by UNESCO, Mount Rinjani would become the first such geological park in Indonesia. It has been claimed that the preliminary documentation required for UNESCO registration has not received sufficient support from the Nusa Teggara Barat government offices. Among the requirements to become a geo-park sufficient information must be supplied to show that the location has sufficient and appropriate management, information services, access to educational instruction to facilitate "knowledge-based geotourism", the implementation of a sustainable regional economy, biodiversity conservation, and to have established public access to the park area.
Mount Rinjani has obtained the World Legacy Award from Conservation International and Traveller (2004), and was a finalist for Tourism for Tomorrow Awards (2005 dan 2008) from the World Travel Tourism Council (WTTC).

Climbing
Track I (east track): [Mataram – Aikmel – Semalun Lawang] – Pos Pemantauan (Ground Base camp) – Pos Tengingian (Tengingian Base Camp) – Pos Padabalong (Padabalong Base Camp) – Plawangan Sembalun – Rinjadi Peak

Track II(south track) : [Mataram – Anyar – Senaru] – Pos I (Base Camp I) – Pos II (Base Camp II) – Pos III (Base Camp III) - Plawangan Senaru – Segara Anak Lake – Plawangan Sembalun – Rinjani Peak.

Track III (northeast track) : [Mataram - Bayan – Torean] – Pos I (Base Camp I) – Kokok Putih – Segara Anak Lake – Plawangan – Sembalun- Rinjani Peak.

Mount Rinjani Picture 


Country: Indonesia 
Subregion Name: Lesser Sunda Islands (Indonesia)
Volcano Number: 0604-03= 
Volcano Type: Stratovolcano Volcano  
Status: Historical 
Last Known Eruption: 2004 
Summit Elevation: 3726 m 12,224 feet 
Latitude: 8.42°S 8°25'0"S 
Longitude: 116.47°E 116°28'0"E

Mount Tambora

Mount Tambora (or Tamboro) is an active stratovolcano, also known as a composite volcano, on the island of Sumbawa, Indonesia. Sumbawa is flanked both to the north and south by oceanic crust, and Tambora was formed by the active subduction zone beneath it. This raised Mount Tambora as high as 4,300 m (14,100 ft), making it formerly one of the tallest peaks in the Indonesian archipelago. After a large magma chamber inside the mountain filled over the course of several decades, volcanic activity reached a historic climax in the super-colossal eruption of April 1815.
The 1815 eruption is rated 7 on the Volcanic Explosivity Index, the only such eruption since the Lake Taupo eruption in about 180 AD. With an estimated ejecta volume of 160 cubic kilometers, Tambora's 1815 outburst was the largest volcanic eruption in recorded history. The explosion was heard on Sumatra island (more than 2,000 km (1,200 mi) away). Heavy volcanic ash falls were observed as far away as Borneo, Sulawesi, Java and Maluku islands. Most deaths from the eruption were from starvation and disease, as the eruptive fallout ruined agricultural productivity in the local region. The death toll was at least 71,000 people (the most deadly eruption in recorded history), of whom 11,000–12,000 were killed directly by the eruption; the often-cited figure of 92,000 people killed is believed to be overestimated. The eruption created global climate anomalies that included the phenomenon known as "volcanic winter": 1816 became known as the "Year Without a Summer" because of the effect on North American and European weather. Agricultural crops failed and livestock died in much of the Northern Hemisphere, resulting in the worst famine of the 19th century.
During an excavation in 2004, a team of archaeologists discovered cultural remains buried by the 1815 eruption. They were kept intact beneath the 3 m (9.8 ft) deep pyroclastic deposits. At the site, dubbed the Pompeii of the East, the artifacts were preserved in the positions they had occupied in 1815.

Geographical Setting
Mount Tambora is located on Sumbawa Island, part of the Lesser Sunda Islands. It is a segment of the Sunda Arc, a string of volcanic islands that forms the southern chain of the Indonesian archipelago. Tambora forms its own peninsula on Sumbawa, known as the Sanggar peninsula. At the north of the peninsula is the Flores Sea, and at the south is Saleh Bay, 86 kilometres (53 mi) long and 36 kilometres (22 mi) wide. At the mouth of Saleh Bay there is an islet called Moyo (Indonesian: Pulau Moyo)
Besides its interest for seismologists and volcanologists, who monitor the mountain's activity, Mount Tambora is an area of scientific studies for archaeologists and biologists. The mountain also attracts tourists for hiking and wildlife activities. The two nearest cities are Dompu and Bima. There are three concentrations of villages around the mountain slope. At the east is Sanggar village, to the northwest are Doro Peti and Pesanggrahan villages, and to the west is Calabai village.
There are two ascent routes to reach the caldera. The first route starts from Doro Mboha village southeast of the mountain. This route follows a paved road through a cashew plantation until it reaches 1,150 metres (3,770 ft) above sea level. The end of this route is the southern part of the caldera at 1,950 metres (6,400 ft), reachable by a hiking track. This location is usually used as a base camp to monitor the volcanic activity, because it only takes one hour to reach the caldera. The second route starts from Pancasila village northwest of the mountain. Using the second route, the caldera is accessible only by foot.

Ecosystem

A scientific team led by a Swiss botanist, Heinrich Zollinger, arrived on Sumbawa in 1847. Zollinger's mission was to study the eruption scene and its effects on the local ecosystem. He was the first person to climb to the summit after the eruption. It was still covered by smoke. As Zollinger climbed up, his feet sank several times through a thin surface crust into a warm layer of powder-like sulfur. Some vegetation had re-established itself and a few trees were observed on the lower slope. A Casuarina forest was noted at 2,200–2,550 m (7,200–8,370 ft). Several Imperata cylindrica grasslands were also found.
Rehabitation of the mountain began in 1907. A coffee plantation was started in the 1930s on the northwestern slope of the mountain, in the village of Pekat. A dense rain forest, dominated by the pioneering tree, Duabanga moluccana, had grown at an altitude of 1,000–2,800 m (3,300–9,200 ft). It covers an area up to 80,000 hectares (800 km2). The rain forest was explored by a Dutch team, led by Koster and de Voogd in 1933. From their accounts, they started their journey in a "fairly barren, dry and hot country", and then they entered "a mighty jungle" with "huge, majestic forest giants". At 1,100 metres (3,600 ft), they entered a montane forest. Above 1,800 metres (5,900 ft), they found Dodonaea viscosa dominated by Casuarina trees. On the summit, they found sparse Anaphalis viscida and Wahlenbergia.
In 1896, 56 species of birds were found, including the Crested White-eye. Twelve further species were found in 1981. Several other zoological surveys followed, and found other bird species on the mountain, resulting in over 90 bird species discovered on Mount Tambora. Yellow-crested Cockatoos, Zoothera thrushes, Hill Mynas, Green Junglefowl and Rainbow Lorikeets are hunted for the cagebird trade by the local people. Orange-footed Scrubfowl are hunted for food. This bird exploitation has resulted in a decline in the bird population. The Yellow-crested Cockatoo is nearing extinction on Sumbawa island.
Since 1972, a commercial logging company has been operating in the area, which poses a large threat to the rain forest. The logging company holds a timber-cutting concession for an area of 20,000 hectares (200 km2), or 25% of the total area. Another part of the rain forest is used as a hunting ground. In between the hunting ground and the logging area, there is a designated wildlife reserve where deer, water buffalos, wild pigs, bats, flying foxes, and various species of reptiles and birds can be found.
Country:IndonesiaSubregion Name:Lesser Sunda Islands (Indonesia)Volcano Number:0604-04=Volcano Type:StratovolcanoVolcano Status:HistoricalLast Known Eruption: 1967 ± 20 years Summit Elevation:2850 m 9,350 feetLatitude: 8.25°S 8°15'0"SLongitude:118.00°E118°0'0"E

Country: Indonesia
Subregion Name: Lesser Sunda Islands (Indonesia)
Volcano Number: 0604-04=
Volcano Type: Stratovolcano
Volcano Status: Historical
Last Known Eruption: 1967 ± 20 years 
Summit Elevation: 2850 m 9,350 feet
Latitude: 8.25°S 8°15'0"S
Longitud: 118.00°E118°0'0"E

Monday, September 20, 2010

Mount Merbabu

Mount Merbabu (Indonesian: Gunung Merbabu) is a dormant stratovolcano in Central Java province on the Indonesian island of Java. Loosely translated, Gunung Merbabu could mean 'Mountain of Ash' from the Indonesian word abu. The active volcano Mount Merapi is directly adjacent on its south-east side, while the city of Salatiga is located on its northern foothills. A 1,500m high broad saddle lies between Merbabu and Merapi, the site of the village of Selo and highly fertil farming land.

There are two peaks; Syarif (3,119 m) and Kenteng Songo (3,145 m). Three U-shaped radial valleys extend from the Kenteng Songo summit in northwesterly, northeastly and southeastly directions.
Two known moderate eruptions occurred in 1560 and 1797. The 1797 event was rated 2: Explosive, on the Volcanic Explosivity Index. An unconfirmed eruption may have occurred in 1570.
Geologically recent eruptions originated from a North Northwest-South Southeast fissure system that cut across the summit and fed the large-volume lava flows from Kopeng and Kajor craters on the northern and southern flanks, respectively.

Merbabu can be climbed from several routes originating from the town of Kopeng on the north east sideside, and also from Selo on the southern side. A climb from Kopeng to Kenteng Songo takes between 8 and 10 hours.
An area of 57 km² of the mountain has been declared a national park in 2004.

Merbabu Track 
Track I (south track) : [Salatiga – Kopeng – Takelan] – Pos Pending (Pending Base Camp) – Pos I (Base Camp I) Gumuk – Pos II (Base Camp II) Lempong Sampan – Pos III (Base Camp III) Watu Gubuk - Pos IV (Base Camp IV) Watu Tulis – Pos V (Base Camp V) Helipad – Kenteng Songo Peak

Track II (west track) : [Magelang – Kaponan – Wekas] – Pos I (Base Camp I) – Pos II (Base Camp II) – Pos Helipad (Helipad Base Camp) – Kenteng Songo Peak

Track III (south track) : [Surakarta - Cepogo – Selo] – Tarubatang – Pos I (Base Camp I) Balong – Pos II (Base Camp II) Pentur – Pos III (Base Camp III) – Kenteng Songo Peak


 Mount Merbabu Picture 1

 Mount Merbabu Picture 2

 Mount Merbabu Picture 3


Country: Indonesia 
Subregion Name: Java (Indonesia) 
Volcano Number: 0603-24= Volcano
Type: Stratovolcano 
Volcano Status: Historical 
Last Known Eruption: 1797 
Summit Elevation: 3145 m 10,318 feet 
Latitude: 7.45°S 7°27'0"S 
Longitude: 110.43°E 110°26'0"E

Sunday, September 19, 2010

Mount Agung - Bali

Mount Agung or Gunung Agung is a mountain in Bali, Indonesia. This stratovolcano is the highest point on the island. It dominates the surrounding area influencing the climate. The clouds come from the west and Agung takes their water so that the west is lush and green and the east dry and barren.
The Balinese believe that Mount Agung is a replica of Mount Meru, the central axis of the universe. One legend holds that the mountain is a fragment of Meru brought to Bali by the first Hindus. The most important temple on Bali, Pura Besakih, is located high on the slopes of Gunung Agung.
Gunung Agung last erupted in 1963-64 and is still active, with a large and very deep crater which occasionally belches smoke and ash. From a distance, the mountain appears to be perfectly conical, despite the existence of the large crater.
From the peak of the mountain, it is possible to see the peak of Mount Rinjani on the island of Lombok, although both mountains are frequently covered in clouds.

The 1963-64 Eruption
On February 18, 1963, local residents heard loud explosions and saw clouds rising from the crater of Mount Agung. On February 24, lava began flowing down the northern slope of the mountain, eventually traveling 7 km in the next 20 days. On March 17, the volcano erupted (VEI 5), sending debris 8–10 km into the air and generating massive pyroclastic flows. These flows devastated numerous villages, killing approximately 1500 people. Cold lahars caused by heavy rainfall after the eruption killed an additional 200. A second eruption on May 16 led to pyroclastic flows which killed another 200 inhabitants.
The lava flows missed, sometimes by mere yards, the Mother Temple of Besakih. The saving of the temple is regarded by the Balinese people as miraculous and a signal from the gods that they wished to demonstrate their power but not destroy the monument the Balinese faithful had erected.

Climbing the Mountain
There are two routes up the mountain, one from Besakih which proceeds to a higher peak and starts at approximately 1,100 m (3,610 ft) and another which commences higher from Pura Pasar Agung, on the southern slope of the mountain, near Selat and which is reputed to take four hours. There is no path between the two routes at the top. Cecilie Scott provides an account of the ascent from Pura Pasar Agung. Greg Slayden describes a climb from Besakih claimed to have taken a remarkable four and a half hours to the peak and Ken Taylor that took much longer and which included getting lost.
Guides are available in Besakih and the mountain can also be climbed without a guide. The climb from Besakih is quite tough. It is sometimes tackled as a single climb generally starting about 10.00pm for a dawn arrival at the peak and sometimes with an overnight camp about three quarters of the way up. It is far harder than the more popular Balinese climb up Gunung Batur. It is not a mountain that needs ropes and not quite high enough for altitude sickness but adverse weather conditions develop quickly and warm waterproof clothing is required and should be carried. There is no water available along the route.
Proceed through the temple complex then continue on a path that travels continuously upwards on a steep narrow spur through open forest and jungle most of the way. There is little potential to get lost until the route opens up towards the top where the correct route doubles backwards. Many climbers miss this turn and continue up a small valley which can be climbed out of with some difficulty.

Climbing
Mount Agung peak can to reach passing three route, southeast route from Budakeling passing Nangka, south track passing Sangkan Kuasa and southwest route, the most popular and save track : [Denpasar – Batubulan – Besakih] – Hutan Pengubengan – Agung Peak
Mount Agung Picture 1

Mount Agung Picture 2

Mount Agung Picture 3
 
Country: Indonesia
Subregion Name: Lesser Sunda Islands (Indonesia)
Volcano Number: 0604-02=
Volcano Type: Stratovolcano
Volcano Status: Historical
Last Known Eruption: 1964
Summit Elevation: 3142 m 10,308 feet
Latitude: 8.342°S 8°20'30"S
Longitude: 115.508°E 115°30'30"E