M Bali Tour

Departure from hotel: 08.30 am

Bali Cheaper Price:
USD 55 / CAR (Max 6 Persons) / IDR 500.000
USD 100 /Mini Bus (Max 12 Persons) / IDR 900.000

M Bali Tours - First stop in Kuta to see the Barong dance which has

become a symbol of Bali's history, ticket prices USD 9 for the duration of the event for 1 hour, starting at 9:00 to 10:00 am. then, continue our journey to the village of art: Batubulan (Batik / hand woven clothing), Celuk (Gold and Silver production), Batuan (painting) and the last art village is the village of Mas (woodcarving). after the village of art, we'll invite you to drink in coffee plantations (famous with Luwak Coffee / Pea Berry Coffee / Coffee from animal) in the village of Oka friends in the Garden (Civet coffee and five types of beverages). Lunch with the beauty of Mount and Lake Batur in Kintamani.
after lunch at Kintamani, we direct to Besakih (mother temple), after the Besakih us back to the hotel.

Note :
Bali Cheaper Price for Lunch at restaurant on the hill in Kintamani (Volcano) USD 8 / person.

History of Mount Agung:

Gunung Agung is also the ancient name for Mount Slamet

in Java.

Mount Agung is the highest mountain on the island of Bali with a height of 3142 masl. The mountain is located in the district of Rendang, Karangasem regency, Bali.

Gunung Agung is a volcano stratovolcano, this mountain has a very large crater is very deep and sometimes smoke and water vapor. Pura Besakih From this mountain with a conical taper seems perfect, but the actual peak of this mountain elongated and ends in a circular craters and wide.
From the top of Mount Agung we can see the peak of Mount Rinjani in Lombok Island in the east, although both mountains covered with clouds because both peaks are above the clouds, the islands of Nusa Penida in the south and its beaches, including beach and mountain Sanur and Lake Batur in the northwest.

Hindu community trust

Balinese Hindu community believe that Mount Agung is the place bersemayamnya Gods - Gods, and also society believe that these mountains there is the palace of the gods. Therefore, the Balinese community to make this place as a place that purified Kramat.

ERUPTION HISTORY

The eruption of Mount Agung is known as much as 4 times since 1800, as shown in Table 3.

Table 3.

NOTE: The eruption of Mount Agung

Year eruption	Activity
1808	In this year hurled ash and pumice with a number of extraordinary
1821	Normal eruption, then no information
1843	The eruption was preceded by earthquakes. Material that is spewed out ash, sand and pumice. Subsequently in 1908, 1915, and 1917 in various places in the bottom of the crater and looked copies dike fumarola.
1963	The eruption began staircase February 18, 1963 and expire on January 27, 1964. The eruption is magnatis. The victim was recorded 1148 people died and 296 people injured.

Character Explosion

Patterns and distribution of the results of past eruptions prior to 1808, 1821, 1843, and 1963 show a similar type of eruption, such as explosive (eruption, with a cast incandescent rocks, pieces of lava, pyroclastic and ash rain), and the effusive form of pyroclastic flow , and lava flows (Sutukno B., 1996).

Period Eruption

Of the four events of the past eruptions, periods of rest Gunung Agung can be seen that the shortest of 16 years and the longest 120 years, as shown in the table below.

Gunung Agung rest period

Year of Explosion	Rest Period (years)
1805
1821	16
1843	22
1963	120

Eruption 1963

Chronology of eruption of 1963

Old eruption of Mount Agung in 1963 lasted almost a year, from mid February 1963 to January 26, 1964, with the chronology as shown in Table 5.

Table 5. Chronology of the eruption in 1963

Time	Activity
16 Pebruari 1963	Mild earthquakes felt by residents of several Kampung Yekhori (lk. 928 m from sea level) on the southern slope, approximately 6 km from the summit of Mount Agung.
17 Pebruari 1963	Earthquake Felt in the village of Kubu in the Foothills northeast coast at a distance lk. 11 km from the crater hole
18 Pebruari 1963	At approximately 23:00 on the north coast voice thundering in the soil
19 Pebruari 1963	At 01.00 looks smoke and smell sulfur gas 03.00 seen clouds that waft from the crater, the more great clotted - blob and two hours later began a loud boom sounded for the first time. The voice that resonates long time this was followed by a blast of rock fist and terminated by a burst of smoke gray blackish. A bomb from a distance looking for coconuts apart from the others and hurled through the peak towards Besakih. Village Residents Sebudi and Jackfruit in the southern slope began to evacuate, especially not the surrounding air resistance that started hot and it smelled of sulfur. In the vicinity of More, the air filled with mist, while the ash began to fall. The water in the river began to fall. The water in the river has been colored brown and viscous bring rock with a roar, marks the beginning of the lava rain. Residents to remain calm and do the praying. At 10.00 there was another cracking noise and the smoke getting thicker. Unobstructed views toward the mountain fog, moderate rain began to fall in the mud around its slopes. At night the flames visible movement at the mouth of the crater, while the lightning connection - connecting over the top.
20 Pebruari 1963	Mountain volcano still shows movement 06:30 sound throws a bomb explosion and looks bigger. 07:30 Kubu people started to panic, many of them fled to Tianyar, while residents of the south slope and moved to Bebandem Strait.
21 Pebruari 1963	Thick smoke still billowed from the crater. 12.30 leleran lava looks north toward the tension
22 Pebruari 1963	Activities continue in the form of an eruption of smoke and flames leap and roar.
23 Pebruari 1963	0830 around Besakih, Rendang and bombarded the Strait of small and sharp stones, sand and ash.
24 Pebruari 1963	Heavy rain fell in the mud Besakih cause Eka Dasa Rudra several buildings collapsed. Temukus residents fled to Besakih. Pyroclastic eruption fell through Tukad Power to the tension.
25 Pebruari 1963	At 15.15 heat clouds down in the northeast through Tukad Barak and Power. Rain on Lava T. Power causes the relationship between faction and Tianyar disconnected. Village Bantas - Siligading hit by hot clouds resulted in 10 people victims. Lahar rain hit 9 units in the village of Ban's house, the victim of 8 people.
26 Pebruari 1963	Lava in the north still wander. Rain lava flows until at Village Sogra, Sangkan Authorization. The smoke seemed to rise and the population Sogra Village, sangkan Counsel, Badeg hamlet and middle Badeg fled to the south. More rain in a rather thick and itchy down. Lahar happening around Sidemen. Also lava flows in the north in T. Power and T. Barak. At 18:15 the rain of sand in Besakih. Pangi air filled with the sharp sulfur sekali.Penduduknya Babandem refuge. Then the activities of G. Great is constantly in progress, virtually every day of ash raining down, while the river flowing lava and lava continued to wander to the north.
17 Maret 1963	Is the peak activity. High eruption cloud reached a climax at 5:32. At the moment seemed to cloud observations of eruptions under Rendang had passed the Zenith and this situation lasted to 13.00. Heat clouds down and go into T. Yehsah, T. Langon, T. Barak and T. Janga in the south. In the north of the mountain since the eruption of voices heard at 01.00 on average once every five seconds. Heat clouds down toward the lumpy T. Sakti, T. Power and other rivers in the north. Beginning at 7:40 rain lahar occurred white smoke, and it lasted until around 8:10. 08.00 raining ash, at 09:20 rained gravel, and while it's hot clouds had come down bumpy. At 11:00 increasingly heavy ash rain until completely unobstructed vision. At 12.00 a smoky white lava began to overflow from the edges of T. Power. New ash rain let up at 12.45 and then at 15.30 the cracking noise was further reduced to disappear altogether. The river is conceded hot clouds during the peak of this activity is as much lk. 13 and 7 on the southern slopes of fruit on the slopes of the north. Farthest distance reached is lk.14 km, is in T. power in the north. The western and eastern mountain cloud-free summer. The duration of first place this cataclysmic ie during lk. 10 hours ie from 05.00 till 15.00.
21 Maret 1963	City Subagan, Karangasem rain pounded lava until fall victim lk. 140 people. After the massive eruption on 17 March, then the activity decreased, while the roar that was heard continuously vanish away. So leleran lava to the north stopped at line height and reach distance of 501.64 m lk. 7290 m from the summit.
16 Mei 1963	The cataclysmic eruption of both preceded by an introduction, at first weak and is slowly getting stronger. On the afternoon of May 16, activity increased again and hold meneru, until it reaches its peak at 17:07. In general, the power of the eruption peaked for the second time is not as good as the first. Eruption cloud reached a height lk. 10,000 m at the summit of power, at 17:15 o'clock lapili rain began to fall until around 21:13. River which conceded hot cloud is 8 units, 6 in the south and 2 north. Farthest distance reached lk. 12 km that is in Tukad nauseating, feet south. The duration lasts cataclysmic lk. 6 hours, ie from 16 pm until around 21:00. In general, the power of the eruption peaked for the second time is not as good as the first. Eruption cloud reached a height lk. 10,000 m at the summit of power, at 17:15 o'clock lapili rain began to fall until around 21:13. River which conceded hot cloud is 8 units, 6 in the south and 2 north. Farthest distance reached lk. 12 km that is in Tukad nauseating, feet south. The duration lasts cataclysmic lk. 6 hours, ie from 16 pm until around 21:00.
Nopember 1963	High smoke solfatara / fumarola reach lk. 500 m at the peak ats. Since November the eruption of smoke color is white.
10 Januari 1964	High gusts of smoke up to 1,500 m above the summit
26 Januari 1964	At 6:50 of smoke visible from the summit of Mount Agung gray and then at 07:02, 07:05 and 07:07 appear more similar eruptions of thick black smoke cauliflower, following one after another of the three holes, at first from the west and the east to reach the maximum height lk . 4,000 m above the summit. The entire edge of the crater appears covered olaeh cloud. The voice sounded weak but bright as well.
27 Januari 1964	Activity of Mount Agung stop.

1963 Eruption Products

Lahar Rain

In accordance with the geographical location of Mount Agung which acts as a rain catcher southeast winds that blow, huge lava begins on the slopes of the north, then east to the southeast on a slope and then gradually shifted to the westward and reach the climax in the south-west slope. Large lava to the south began to spread at an altitude of 500 m between Rendang and padangkerta. Then under T. Jangga, which is in T. Krekuk and Jasi, and finally in T. Bugbug Unda. Given the northern region lies within the rain shadow, not a shadow of lava rather than loose sediment, the actual maximum fall on this side.

Lava Flow

Lava that wander between February 19 and March 17, 1963 flowing from the main crater at the summit to the north, through the lowest edge of the crater, stopping at the line height and reach distance of 505.64 m lk. 7290 m. The contents of the lava is estimated as many as lk. 339.235 million m3.

Material Release

Composed of volcanic bombs, lapili, sand and ash, both derived from pyroclastic eruptions or from the explosion crater center. The number of activities take place entirely over the wheel:

Eflata (bombs, sand and ash) lk. 380.5. 106 m3

ladu lk. 110.3. 106 m3

Total lk. 490.8. 106 m3

Heat G Great Cloud

At Mount Agung, there are two kinds of hot clouds, namely clouds and pyroclastic eruptions hot avalanches. Pyroclastic eruption occurred at the time there is a big eruption. At that time the bottom of the pile is saturated with the eruption of volcanic material beyond the edge of the crater and slid down. Movement through the lower section on the edge of the crater, is a ravine and then follow the stream. The speed of the eruption cloud was observed from the Post Rendang is an average of 60 miles per hour and in the south reached the farthest distance of 13 km, which is in T. Nauseating and 14 km north of the T. Power.

According Suryo (1964) hereinafter, the clouds are glowing hot hot clouds that often slid out from under the peak (the edge of the crater). although there is no eruption pyroclastic avalanches could occur. Can also occur if there part of the still hot lava fall, as happened at the time of lava drip on the north slope.

Areas affected pyroclastic eruption on 1963 activity is limited to the south and north slopes alone, because both the west and the east of the crater there is a punggung.Kedua this back extending from west to east. Pyroclastic eruption that goes beyond the eastern edge of the crater is broken down by the back into two departments are the northeast and southeast. So hot clouds in the west of the west's back is broken by the direction southwest and north. Pyroclastic eruptions that occurred during the 1963 activity have plagued the land area falls 863 lk.70km2 and cause human casualties.

Victims of Great Mountain Activities

According Suryo (1965, p.22-26) there are 3 causes symptoms that led to falling victim during the activities of Mount Agung in 1963, namely due to the hot clouds, pyroclastic and lava. Human casualty data are shown in Table 6.:

Table 6. The number of human casualties

	Jumlah korban (orang)
	meninggal	luka
Awan panas	820	59
Piroklastika	163	201
Lahar	165	36
Jumlah	1.148	296

Another disadvantage

Other Kerugain by the eruption of Mount Agung in 1963 broken down as shown in Table 7 below:

Another loss by the eruption of Mount Agung in 1963

Cause

Type of victim

Cloud heat

Lava
Eflata

54 klasiran and banjo there are a lot of damage.

45 villagers, including 12 pieces destroyed, the rest partially damaged

1963 bush house and hut.

75 ha and 2201.63 ha of paddy fields

1167 head of cattle and 10 918 birds

2567 head of cattle

1382 birds

21 villages, 5 of them were destroyed

4172 home

1359.685 ha of rice and 870 ha of lading

150 head of cattle

2617 birds

1564 houses buried, burnt and damaged

53.983.00 ha field buried

11.745.00 ha of damaged forest

Greatness and Energy

Kusumadinata (1964) have calculated the energy and power of the eruption of Mount Agung in 1963 with the following results:

Grandeur

The volume of eruption

Specific gravity

Heat energy released

Equality atomic bomb

Greatness eruption

: IV (H.Suya, 1955)

: 0,83 km3 (V)

: 2,3 (d)

: 2,189.1025 erg (Eth)

: 2605,9 (Ae)

: 8,99

Diposkan oleh Dexcan

Note :
Bali Cheaper Price for Lunch at restaurant on the hill in Kintamani (Volcano) USD 8 / person.

Bali Cheaper Price :

Departure from the hotel : 8:30 am

Included : Aircon , Petrol , Driver , Guide.

Reservation :

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