Mt. Slamet
PROFILE;
| Maps; Google Map Link |
 (*only for information); |
| Name: |
| Mt. Slamet; Mt Agung [referred to as Mt Agung in a Sundanese manuscript of the adventure of Bujangga Manik is Mount Slamet (J. Noorduyn)] |
| Note: |
| The Dutch historian J. Noorduyn theorizes that the name “Slamet” is relatively new, ie after the entry of Islam into Java (the word is an Arabic loan). He argues that the so-called Gunung Agung in the Sundanese manuscript of the adventure of Bujangga Manik is Mount Slamet, based on the exposure of the mentioned location Crater IV is the last crater that is still active until now, and last active until the level of standby medio-2009.Mount Slamet is formed due to Indo-Australian Plate subduction on the Eurasian Plate in the south of Java Island. Cracks in the plates open the lava path to the surface. Records of eruptions are known since the 19th century. The mountain is active and often has small-scale eruptions.This mountain has a forest area of Dipterocarp Hill, Upper Dipterocarp forest, Montana forest, and Ericaceous Forest or mountain forest. |
| Conservation: |
| Curug Bengkawah Nature Reserve; Guci Nature Reserve; |
GOVERMENT ADMINISTRATION
| Province | Central Java |
| City / Regency |
|
| Distrik | 1.1 Kecamatan Pulosari
2.1 Kecamatan Karangreja; 2.2 Kecamatan Bojongsari; 3.1 Kecamatan Sumbang; 3.2 Kecamatan Baturaden; 3.3 Kecamatan Kedung Banteng 4.1 Kecamatan Bumijawa; 4.2 Kecamatan Bojong |
| Village | 1.1.1 Desa Gunungsari; 1.1.2 Desa Penakir; 1.1.3 Desa Batursari; 1.1.4 Desa Jurang Mangu
2.1.1 Desa Serang; 2.2.1 Desa Bumisari; 3.1.1 Desa Gandatapa; 3.1.2 Desa Limpakuwus; 3.2.1 Desa Kemutug Lor; 3.2.2 Desa Katenger; 3.3.1 Desa Melung 4.1.1 Desa Guci; 4.1.2 Desa Sigedong 4.2.1 Desa Dukuh Tengah; 4.2.2 Desa Kedawung; |
PHISICAL CONDITION
| Shape; |
| Stratovulcano |
| Condition; |
| a vulcano / a active |
| History of eruption; |
| 1772; August 11-12, eruption of ash and lava 1825; October, an ash eruption occurred 1835; September (2 days), an ash eruption occurred 1847; Enhanced activity 1849; December 1, an ash eruption occurred 1860; March 19 and 11 April, an ab eruption 1875; May, June, November and December, an ash eruption occurred 1885; 21- 30 March, an ash eruption occurred 1890; An ash eruption occurred 1904; July 14 – August 9, an ash and lava eruption occur 1923; June, an ash and lava eruption occurred 1926; November (for a week), an ash and lava eruption occurred 1927; February 27, an ash and lava eruption occurred 1928; 20 – 29 March and 8 – May 12, an ash and lava eruption occurred 1929; 6, 7 and 15 June, an ash and lava eruption occurred 1930; 2 – 13 April, eruption of ash and lava 1932; July 1 and September 12, an ash and lava eruption occurred 1934; Increased activity 1939; March 20, late April, May 6, July 15 and December 4, an ash eruption 1940; 15 – 20 March and 15 April, an ash eruption occurred 1943; March 18, 1 – October 10, there is an increase in activity, ash rain and the sound of boom 1944; 5 January, 30 June, July and 28 – 30 October, an increase in activity 1948; 14 November, there was an increase in activity 1949; There was an increase in activity 1951; February 11, June 26, July 2, August 24, October and December 30, an increase in activity 1952; January 1, an increase in activity 1953; July, August and October, an ash and lava eruption occurred 1955; 12 – 13 November, 6 and 16 December, there was an ash and lava eruption 1957; February 8, an ash eruption occurred 1958; 17 April, 4 and 6 May, 5 and 13 September, October, an ash and lava eruption occurred 1960; December, an ash eruption occurred 1961; January, an ash eruption occurred 1966; An ash eruption occurred 1969; June, July and August, an ash eruption occurred 1973; August, there was a burst of lava in the crater 1988; 12 – 13 July, eruption of ash and lava 1989; 9 – end of October, seismicity increases 1990; February 20 – March 29, there is an increase in seismicity 1991; June 28 – July 9, an increase in seismicity 1992; March 12 – April 4, an increase in seismicity 2000; an increase in seismicity 2004; November, blowing tremor 2005; July 21st, blowing tremors 2009; Volcanic activity G. Slamet was raised from Waspada (Level II) to Standby (Level III) on 23 April 2009 at 18:00 WIB. The upgrading of this activity lasted until July 2009 |
| Elevation (meters above sea level); |
| 3.428 m (11.247 ft) |
| Type of eruption; |
| Based on the historical record of the eruption, in general the eruption of Mount Slamet is an ash eruption accompanied bursts of sekoria and incandescent, occasionally issued a lava incandescent. The eruption lasted several days, in extraordinary circumstances reaching a few weeks.
In the event of a major eruption, such as the eruption of Mount Agung (1962), Mount Galunggung (1982) or Mount Colo (1983), the main danger of Mount Slamet eruption or primary hazard (direct hazard due to eruption) is a hot clouds slide, pyroclastic flares (volcanic bomb , lapilli, sand and ash) and possibly lava flows. The secondary hazard (the indirect danger of eruption) is the rain lava that occurs after the eruption when it rains heavily around the peak. The far-reaching distribution of pyroclastic falls, depending on the height of the blast and the wind blowing at the time of the eruption, especially the spread of ash and sand rain. Eruption Period. The eruption of Mount Slamet repeatedly in the tempo, lasting the longest to several weeks (less than a month). The shortest break period between two eruptions lk. 1 year and longest 53 years. For lk break period. 1 year may still be a single phase of eruption or follow-up activity. |
| Topology & Geology; |
| The sedimentary eruption of Mount Slamet from old to young was all quartered, covering tertiary-aged sedimentary rocks. Some of the eruptions of G. Slamet include 5 districts with an area of 1500 km2 consisting of precipitated Piroklastika droppings, lava flows, lava, hot clouds and surface deposits of Alluvial and Flluvial. Generally, the lava deposits found in Mount Slamet are Andesitic.
Geological structure that develops in the area of Mount Slamet and surrounding areas, generally in the form of normal faults are commonly found in the group Slamet Tua. Traces of this fault in the field are found in the form of Breksiasi, scratch fault line, destruction zone, alignment of hills and valleys, straight and steep escape and sharp contact between rock units. Based on the criteria mentioned above, the geological structure that developed in Mount Slamet can be divided into 3 pieces of fault structure are: Normal Fault Jegjeg, Normal Fault Marinating, Normal Fault Mengger, Graben Guci, Normal Si Jambang Fault, Normal Fault Buntu, Normal Fault Mount Gratamba, Normal Karanggondang Fault, Normal Fault Kubangan, Normal Fault of Kalipagu and Normal Fault Gangs. |
| Temperature; |
| Meteorology Climatology and Geophysics Council check… |
OTHER HABITAT
| Lake |
| … |
| River |
| ;… |
Source
| website |
|
| Blog |
|
|
About Author
heropolo
[Indonesian Forest]
English
العربية
简体中文
Nederlands
Français
Deutsch
Bahasa Indonesia
Italiano
日本語
한국어
Português
Русский
Español
Türkçe