Mount Kelud, East Java

Kelud is a volcano in East Java province, Indonesia, which is still active. The mountain is located on the border between Kediri and Blitar, about 27 km east of Karachi city center.

This mountain has erupted repeatedly, both large and small scale. Even the eruption has been started since the 15th century. Eruption that claimed at least 15,000 people.

This volcanic eruption in 1586 claimed the lives of more than 10,000 people. [1] A system to divert the lava flow has been made extensively in 1926 and still serves to this day after the eruption in 1919 claimed the lives of thousands of cold lava floods swept settlements population.

In the 20th century, Mount Kelut recorded eruption in 1901, 1919 (May 1 [2]), 1951, 1966, and 1990. In 2007 the mountain was again increased its activity. This pattern brings the vulcanologist 15 on an annual cycle for the eruption of this volcano.

This volcanic activity increased in late September 2007 and has been continued until November of that year, marked by increasing the temperature of the crater lake water, the increase in seismic tremor, and changes in the crater lake of a greenish color to white turbid. Status "alert" (highest) issued by the Volcanology and Geological Hazard Mitigation since October 16, 2007 which implies the population within a radius of 10 km from the mountain (approximately 135,000 people) living on the slopes of the volcano to evacuate. However, the eruption did not occur.

Having had somewhat subsided, the activity of Mount Kelut back increase since October 30, 2007 with the rapid rise in water temperature volcanic crater lake and shallow seismicity. On 3 November 2007 at around 16:00 of the lake water temperature exceeds 74 degrees Celsius, well above the normal symptoms of the eruption of 40 degrees Celsius, causing the temperature gauge is broken. Vibration amplitude seismic tremor with large (over 35mm) lead supervisory personnel must evacuate, but again no eruption occurred.

Due to the high activity of the new terjdi unique phenomenon in the history of Kelut with the advent of white smoke from the middle of the lake followed by lava dome from the middle of the crater lake since 5 November 2007 and continues to "grow" up to 100m wide size. Experts consider this lava dome that obstruct the channel so that the magma eruption is not imminent. Energy for the eruption of the lava dome is used to drive the rest of the 1990 eruption.

Mount Krakatau (Krakatoa), West Java

Krakatoa is a volcanic island that is still active and located in the Sunda Strait between Java and Sumatra. This name was never pinned on a volcanic peak there (Mount Krakatau) which vanish because of eruptions themselves on 26-27 August 1883. The eruption was so powerful; hot clouds and the resulting tsunami killed about 36,000 people. Until before the date of December 26, 2004, this is a terdahsyat tsunami in the Indian Ocean region. Explosion sound was heard up in Alice Springs, Australia and the island of Rodrigues near Africa, 4653 miles. Yield is estimated at 30,000 times the atomic bomb that was detonated on Hiroshima and Nagasaki at the end of World War II.

The eruption of Krakatoa caused global climate change. The world was dark for two and a half days due to volcanic ash that covered the atmosphere. The sun shines dim until next year. Scattering dust visible in the sky Norway to New York.

The explosion of Krakatoa is actually less than the eruption of Mount Toba and Tambora in Indonesia, Mount Tanpo in New Zealand and Mount Katmal in Alaska. However, the erupting mountains far in the human population is still very little. Meanwhile, when Krakatoa erupted, the human population is dense enough, science and technology has evolved, the telegraph was invented, and submarine cable has been installed. Thus it can be said that while information technology is growing and growing rapidly.

Due to the great explosion, three-quarters of the body were destroyed leaving Ancient Krakatoa caldera (large crater) in the Sunda Strait. The sides or edges of the crater known as Rakata Island, Long Island and Island Sertung, in another record called Pulau Rakata, Rakata Island and Small Island Sertung. The explosion was allegedly responsible for the occurrence of the dark ages of the earth. Bubonic plague occurs as the temperature cools. This plague has significantly reduced the number of people on earth.

The eruption is also considered to be contributing to the expiration of the glory of ancient Persia, the transmutation of the Roman Empire to the Byzantine Empire, the end of the civilization of South Arabia, the extinction of the Mayan city, Tikal and fall of civilizations in South America the Nazca enigmatic. Ancient Krakatoa explosion is expected to last for 10 days at an estimated speed of regurgitated mass reaches 1 million tons per second. The blast shield has formed a thick atmosphere of 20-150 meters, lowering the temperature of 5-10 degrees for 10-20 years.

On the day Monday, August 27, 1883, promptly at 10:20, an explosion on the mountain. By Simon Winchester, a geologist who graduated from the University of Oxford UK is also the author of National Geographic said that the explosion was the biggest, loudest and most devastating volcanic event in modern human history. Eruptions voice heard until 4600 km from the center of the eruption and can even be heard by a 1/8 of the population of the earth at that time.

According to researchers at the University of North Dakota, with the explosion of Krakatoa explosion of Tambora (1815) recorded a value of Volcanic explosivity index (VEI), the largest in modern history. The Guinness Book of Records noted the explosion of Krakatoa as the most powerful explosion in recorded history.

Krakatoa explosion had thrown stones, pumice and volcanic ash with a volume of 18 cubic kilometers. Bursts of dust vulkanisnya mencavai 80 km. Hard objects that flew into the air it falls on the plains of Java and Sumatra, even to Sri Lanka, India, Pakistan, Australia and New Zealand.

The eruption destroyed Danan Mountain, Mount Rakata, and Mount Perbuwatan and some where a half cone is missing, create a basin-wide and 7 km deep as 250 meters. Waves reached as high as 40 meters destroying villages and whatever is on the coast. The tsunami was caused not only because of the eruption, but also the underwater landslide.

Recorded the death toll reached 36 417 people from 295 coastal villages from Merak (Attack) to cilamaya in Karachi, the Cape west coast of Banten to display on the island of Panaitan (Ujung Kulon and southern Sumatra. In Ujungkulon, incoming flood of up to 15 km to the west. next day until a few days later, residents of Jakarta and Lampung outback no longer see the sun. Tsunami waves generated even climbing up to the coast of Hawaii, Central America and the west coast of the Arabian Peninsula seven thousand kilometers away.

Mount Merapi, Central Java

Merapi (peak height of 2968 m above sea level, per 2006) is a volcano in central Java and is one of the most active volcanoes in Indonesia. Slopes of the south side are in the administrative district of Sleman, Yogyakarta, and the rest are in the region of Central Java province, the Magelang district on the west side, Boyolali in the north and east, and Klaten district on the southeastern side. Forest area around the peak became Mount Merapi National Park area since 2004.

The mountain is very dangerous because, according to modern records have erupted (peak activity) every two to five years and is surrounded by very dense settlements. Since 1548, this volcano has erupted 68 times as much. City of Manila and the city of Yogyakarta is the nearest large town, is under 30 km from the summit. On the slopes there is still a settlement to a height of 1700 m and is just four kilometers from the summit. Because of its importance, the Merapi to be one of sixteen volcanoes of the world are included in the Decade Volcano projects (Decade Volcanoes).

Small eruptions occur every 2-3 years, and the larger about 10-15 years. Merapi eruptions recorded a big impact in the year 1006 (allegations), 1786, 1822, 1872, and 1930. Eruption in 1006 made the whole central part of Java island shrouded in ash, based on observations of volcanic ash deposits. Dutch geologist van Bemmelen, theorized that the eruption caused the center of the Kingdom of Medang (Ancient Mataram) should be moved to East Java. Eruption in 1872 is considered as the most powerful eruption in modern geological record with VEI scale is approximately 3 to 4. Latest eruption, 2010, is expected also to have the strength or the same approach. The 1930 eruption, which destroyed thirteen villages and killed 1400 people, is the eruption of the biggest victims of the record until now.

The process of formation of Mount Merapi has been studied and published since 1989 and so on. [3] Berthomier, a French scholar, divided into four stages of development of Merapi. The first stage is the Pre-Merapi (to 400,000 years ago), namely Gunung Bibi parts can still be seen on the east side of the peak of Merapi. Stage occurs when the Old Merapi Merapi began to take shape, but not conical (60000-8000 years ago). Remnants of this stage is Turgo and Bukit Bukit Plawangan in the south, which is formed of basaltic lava. Next is the Middle Merapi (8000 - 2000 years ago), characterized by the formation of high peaks, like Mount Gajahmungkur and Batulawang, which is composed of andesite lava. During the formation process is characterized by lava flows, brecciation of lava and hot clouds. Merapi activity has to be effusive eruptions (molten) and explosive. Also predicted an explosive eruption with material debris left west of the horseshoe morphology with a length of 7 km, 1-2 km wide with a few hills on the western slope. Pasarbubar crater (or Pasarbubrah) thought to be formed at this time. Merapi peak current, peak Anyar, just beginning to form around 2000 years ago. During its development, is known to occur several times an explosive eruption with VEI 4 is based on observations tefra layer.

Characteristics of eruption since 1953 is the insistence of lava to the summit crater is accompanied by periodic lava dome collapse and pyroclastic formation (nuee ardente) which can slide on the slopes or vertically upwards. The eruption of Merapi type is generally not a sound but the hiss of the explosion. Top of the dome there until 2010 was the result of a gas explosion took place since 1969. 

Geologists in 2006 detected a giant space beneath Merapi containing material such as mud that is "significantly impede the vibration waves earthquakes". Scientists estimate that the magma material.  The bags are part of the magma that formed due to the formation of Indo-Australian Plate menghunjamnya under the Eurasian Plate.

Mount Semeru, East Java

Semeru or Mount Sumeru is the highest volcano in Java, with Mahameru peak, 3676 meters above sea level (masl). Crater at the summit of Mount Semeru known Jonggring Saloko. Semeru has a hill dipterocarp forest, dipterocarp forest Upper Montane forest, and forest Ericaceous or mountain forests. The position of this mountain lies between the administration and Lumajang Malang Regency, with its geographical position between 8 ° 06 'S and 120 ° 55' East Longitude.

In 1913 and 1946 Crater Jonggring Saloka have dome with a height of 3744.8 M until the end of November 1973. The south, the dome is to break the edge of the crater caused lava flow leads to the south including the Pronojiwo and Candipuro in Lumajang.

According to Javanese belief that ancient book written in Tantu performances from the 15th century, in ancient times the island of Java floating in a vast sea, tossed around and constantly shaking. The Gods decided to tack the island of Java by moving the Mount Meru in India to the island of Java.

Lord Vishnu transformed into a giant tortoise on his back holding the mountain, while Brahma was transformed into a long snake that wraps his body on the mountain and the mountain tortoise so it can be transported safely.

Gods of the mountain laid on top of the first part of the island they encountered, namely in the western part of Java Island. But the weight of the mountain that resulted in the eastern end of the island rose into the air. Then they move to the eastern part of Java island. When taken to the east of Mount Meru, Mount Meru, the scattered pieces create a line of mountains on the island of Java that extends from west to east. However, when the peak Meru moved to the east, the island of Java is still skewed, so the gods decided to cut some of the mountain and place it in the northwest. This fragment formed Pawitra Mountain, which is now known as Mount Pananggungan, and the main part of Mount Meru, the dwelling place of Lord Shiva, now known as Mount Sumeru. At Sang Hyang Shiva came to the island of Java millet saw many trees, so the island is called Java.

Geographical environment of the island of Java and Bali are matched with Hindu religious symbols. In Hinduism there is the belief of Mount Meru, Mount Meru is considered as the home where dwell the gods and as a means of liaison between the earth (human) and Heaven. Many Javanese and Balinese society today still regard the mountain as the abode of the Gods, Hyang, and spirits.

According to the Bali Mount Mahameru believed to be the father of Mount Agung in Bali and respected by the people of Bali. Ceremonial offerings to the gods of Mount Mahameru conducted by the Balinese. However ceremony conducted only once every 8-12 years at the time people just accept the magical voice of the gods of Mount Mahameru. In addition to the offering ceremonies that the Balinese people often come to the Cave Widodaren to receive the holy Tirta.

Mount Tambora, Sumbawa

Mount Tambora is an active stratovolcano located on the island of Sumbawa, Indonesia. The mountain is located in two districts, namely District Dompu (some distance south to the northwest side, and Bima (south side of the slope to the northwest, and feet to the top of the east to the north), West Nusa Tenggara Province, on 8 ° 15 'S and 118 ° east. mountain is located in both the north and south sides of the oceanic crust. Tambora was formed by the subduction zone beneath. This increases the height of Tambora up to 4,300 m which makes this mountain was once one of the highest peak in archipelago and drain large magma chamber inside the mountain. It took centuries to refill the magma chamber.

This volcanic activity reached its peak in April 1815 when it erupted in a scale of seven on the Volcanic explosivity index. To the eruption's largest eruption since the eruption of Lake Taupo in the year 181. The explosion was heard up to the island of Sumatra (more than 2,000 km). Volcanic ash falls in Kalimantan, Sulawesi, Java and Maluku. The explosion was caused by the death of no fewer than 71,000 people were killed by 11000-12000 direct result of the eruption. In fact, some researchers estimate that up to 92,000 people were killed, but this figure is questionable because based on estimates that are too high. Moreover, the eruption is causing global climate change. The next year (1816) is often referred to as the Year Without a Summer because of the drastic change of weather North America and Europe because of the dust produced from the eruption of Tambora this. Due to drastic climate change is a lot of crop failure and livestock deaths in the Northern Hemisphere which led to the worst famine in the 19th century.

The eruption of Mount Tambora in 1815 there are on a scale of 7. That means very destructive. Explosion of Tambora Sumbawa and making the area around it in the dark. Tens of thousands of people died in the eruption, tsunami, followed later, famine and disease. Strength of the eruption of Tambora was the largest ever recorded in history. Atmospheric vent burst of heat and climate change. There was no summer in 1816 in Europe and North America - 'the year without summer'. Tambora down into the ground a few thousand feet, leaving a large crater at the summit.

According to geological investigation, a high volcanic cone was formed before the eruption in 1815 with similar characteristics to the shape of the hole reached 60 stratovolcano. The hole often emits lava flowing down regularly with a swift to steep slopes.

Since the eruption in 1815, at the very bottom there are deposits of lava and pyroclastic material. Approximately 40% of the layer is represented by 1-4 m of lava flows produced by the thin fragmentation. Scoria thin lava flows. At the top, covered by lava scoria, tuff and pyroclastic rocks that flow into down. In Mount Tambora, there are 20 craters. Some craters have a name, for example Tahe (877 m), Molo (602 m), Kadiendinae, the Dome (1648 m) and Doro Api Toi. The crater is also producing basalt lava flows.

Mount Bromo, East Java

Mount Bromo is one of the still active volcano, Mount Bromo in East Java province. This place is always crowded into a tourist destination because of this mountain has a very attractive natural exoticism, one of which is a vast sea of sand. Bromo has a height of 2392 meters above sea level is located in four regions, namely Probolinggo, Pasuruan, Lumajang, and the District of Malang. This sea of ​​sand in the mountains about ten square meters, this makes the scenery is so amazing, so many local and foreign tourists who traveled purposely to enjoy this natural beauty. Mount Bromo has a crater with a diameter of ± 800 meters (north-south) and ± 600 meters (east-west). While the danger area of a circle with a radius of 4 km from the center of the crater of Bromo.

For residents of Bromo Tengger tribe, Mount Brahma (Bromo) believed to be a sacred mountain. Once a year the community held a ceremony Yadnya Tengger Kasada or Kasodo. This ceremony is held at a temple located at the foot of Mount Bromo and proceed north to the top of Mount Bromo. The ceremony was held at midnight to early morning every full moon around 14 or 15 in Kasodo (tenth) according to the Javanese calendar.

During the twentieth century, the mountain is famous as a tourist spot that erupted three times, with regular time intervals, namely 30 years. Largest eruption occurred in 1974, while the last eruption occurred in 2010.

Bromo eruption history: 2011, 2010, 2004, 2001, 1995, 1984, 1983, 1980, 1972, 1956, 1955, 1950, 1948, 1940, 1939, 1935, 1930, 1929, 1928, 1922, 1921, 1915, 1916, 1910, 1909, 1907, 1908, 1907, 1906, 1907, 1896, 1893, 1890, 1888, 1886, 1887, 1886, 1885, 1886, 1885, 1877, 1867, 1868, 1866, 1865, 1865, 1860, 1859, 1858, 1858, 1857, 1856, 1844, 1843, 1843, 1835, 1830, 1830, 1829, 1825, 1822, 1823, 1820, 1815, 1804, 1775, and 1767.

Mount Kerinci, Padang

Mount Kerinci is the highest mountain in Sumatra, Indonesia's highest volcano, the highest peak in Indonesia and outside Papua. Mount Kerinci is located in Bukit Barisan Mountains, near the west coast, and is located about 130 km south of Padang. The mountain is surrounded by dense forests of Kerinci Seblat National Park and is a habitat for Sumatran tigers and Sumatran rhino.

Summit of Mount Kerinci is at an altitude 3805 meters above sea level, here we can see in the distance stretches a beautiful view of the city of Jambi, Padang and Bengkulu. Even the vast Indian Ocean can be seen clearly. Mount Kerinci has a crater of 400 x 120 meters and contains water that is green. To the east there is a lake Bento, the highest clear watery swamp in Sumatra. Behind him are seven mountains with a beautiful crater almost untouched. Mount Kerinci volcano is a stratovolcano-type is still active and last erupted in 2009.

Mount Kerinci cone-shaped with a width of 13 km (8 miles) long and 25 km (16 miles), stretching from north to south. At its peak in the northeast there is a crater as deep as 600 meters (1969 feet) of water is green. Until now, the crater-sized 400 x 120 meters is still active status.

Mount Kerinci is included in the section of the Kerinci Seblat National Park (TNKS). TNKS is a conservation area which has an area of ​​1.48465 million hectares and is located in the four provinces, which are mostly located in Jambi area. TNKS itself is part of the Bukit Barisan Mountains that extends from north to south on the island of Sumatra.

Mount Arjuna, Malang

Mount Arjuna included in this type of volcano is a mountain of old and inactive, while the mountains fall into the category Welirang active volcano with the persistence of activity in the presence of an active crater sulfur fumes condensed sulfur. Although still in the same circuit, but the mountains and mountain Welirang Arjuno different. On climbing trips in the valley and the slopes around the mountain Arjuna, there are dozens of ancient relics scattered and not abandoned, still largely covered bushes and the ground hard. In recent ascent was unfortunate, many relics of ancient objects of high historical value, not necessarily gone missing.

Arjuno (or Mount Arjuna, the ancient name) is located in Malang, East Java, Strato-type with a height of 3339 m above sea level and is under the management Tahura Soeryo Raden. This mountain is usually achieved from three-point hike is well known that from the Lawang, Tretes and Stone. Arjuno name comes from one of the puppet characters Mahabharata, Arjuna.

Arjuno can climb mountains and a variety of directions, the direction of North (Tretes) via Mount Welirang, and the east (Lawang) and from the west (Stone-Selecta), and the south (Karangploso), also from Sumberawan, Singosari. Sumberawan village is the village handicraft center in the district Singosari, Malang and is the last village to prepare before starting the ascent. Can also pass more easily bypassed Purwosari, because only half an hour from the road and straight to the Tambakwatu.

Mount Rinjani, Lombok

Mount Rinjani is a mountain located on the island of Lombok, West Nusa Tenggara. Mountain which is the second highest volcano in Indonesia with an altitude of 3726 m above sea level and is located at latitude 8 º 25 'S and 116 º 28' E is a favorite for mountain climbers Indonesia because of the beauty of the landscape. This mountain is part of the Mount Rinjani National Park has an area of ​​approximately 41 330 ha and will be proposed the addition to be 76 000 ha to the west and east.

Mount Rinjani with the highest point 3726 m above sea level, dominating most of the views of the northern island of Lombok.

In the west there Rinjani caldera cone with an area of ​​approximately 3500 m × 4800 m, extends towards the east and west. In this there is Segara Anak caldera (soon = sea, lake) covering 11 million square meters with a depth of 230 m. The water that flows from this lake to form a very beautiful waterfall, flowing through a steep ravine. At Segara Anak many carp and tilapia are so often used for fishing. The southern part of the lake is called Segara Endut.

On the east side of the caldera there are New Mount (or Mount Barujari) which has a crater measuring 170m x 200 m with a height of 2296-2376 m above sea level. This small mountain last active / erupted from the date of May 2, 2009 and during May, after the previous eruption in 2004 also. If the eruption of 2004 no casualties, the 2009 eruption has indirectly claimed the lives of 31 people, a flash flood on the crowing (River) Tanggek urging of lava into the Segara Anak. Previously, Mount Barujari ever recorded erupted in 1944 (and establishment), 1966, and 1994.

Mount Agung, Bali

Mount Agung (3142 masl), is the highest mountain on the island of Bali, located between the District of Rendang, Karangasem regency, Bali. Mount Agung is included in the ranks in the form of stratovolcano volcano, the mountain has a fairly large craters are still visible and the smoke and steam. Exact coordinates of the location at 8 ° 342 'S and 115 ° 508' longitude.

Ascent to the summit of this mountain can be started from three different route, namely:

1.     From south of the strait through sangkan is power.
2.     From the east is from Budakeling by jackfruit
3.     Of which Southwestern is a route commonly used by hikers that of Pura Besakih.

Route through the Pura Besakih is a common pathway / normal are mostly selected by the climbers. Through this path you will get a view of Mount Agung treats impressive of all the way. Will also see local people who regularly worship at Pura Besakih, glorify the name of the Lord in places of worship are quite famous.

Passes through Pura Besakih, the climbers are expected to prepare an adequate water supply much, because along the way is not available an adequate water source. Although in the last frontier there is a spring, but is not permitted to be taken because the eyes purify the water in the local community as a sacred place for ritual worship.

Pura Besakih pass route, you will pass through the paths that are relatively narrow, if passed other climbers or less coincide so that the community feels a need to give in order not to collide. More-over if bumped into people who are in a procession carrying a wide range of offerings for their religious worship ceremonies. Before you make the climb you need to know about the important schedules their religious ceremonies, it is better to delay a day or two day schedule of the need to push yourself. Besides the ritual and respect local customs, the way you will not be much disturbed because they have often beat by a convoy.