Indonesian Floral Emblem

Lambang Bunga Nasional Indonesia

Bunga Melati (Jasminum sambac)
Jasminum sambac (syn. Nyctanthes sambac) is a species of jasmine native to southwestern and southern Asia, in the Philippines, India, Myanmar and Sri Lanka.
Common names include Arabian Jasmine, Full (فل) (Arabic), Bel/Beli (Bengali), Mogra (Hindi and Marathi), Mallikā (Sanskrit), Kampupot, Melati (Malay andIndonesian Language), Sampaguita (Filipino), Mallepuvvu (Telugu), Mallikaipu (Tamil), dundu Mallige (Kannada) and Kaliyan (Urdu). The botanic name sambac is derived from a misapplication of the Sanskrit name champaka, which refers to the fragrant flowered shrub Michelia champaca.It is an evergreen vine or shrub reaching up to 1-3 m tall. The leaves are opposite or in whorls of three, simple (not pinnate, like most other jasmines), ovate, 4-12.5 cm long and 2-7.5 cm broad. The flowers are produced in clusters of 3-12 together, strongly scented, with a white corolla 2-3 cm diameter with 5-9 lobes. The flowers open at night, and close in the morning. The fruit is a purple-black berry 1 cm in diameter.
flower is known as sampaguita and was adopted by the government as its national flower in 1937. Filipinos string the flowers into leis, corsages and crowns and distill its oils and sell them in stores, streets, and outside churches. The garlands may be used to welcome guests, or as an offering or adornment in religious altars. Its oil is believed to be a cure for headache.
In Cambodia, the flower is used as an offering to the Buddha. Since 96.5% of Cambodians are Buddhists, it is widely known throughout the country. The season of the flower begins in June, the month that provides the most rain. During this month, many civilians thread the flower buds onto a wooden needle to be presented to the Buddha.
In Bengali, the flower is known as beli and is extremely popular for its sweet fragrance. It is used to make garlands to adorn women's hair. And in South India, too, they are strung into thick strands and worn as a hair adornment. In Hawaii, the flower is known as pikake, and is used to make fragrant leis.
In China, the flower is processed and used as the main ingredient in jasmine tea.


Bunga Anggrek Bulan (Moon Orchid)
Phalaenopsis amabilis, commonly known as the Moon Orchid, is a species of orchid.
It was first discovered on a small island off the east coast of New Guinea by native botanist Georgius Everhardus Rumphius in 1653; however, he named itAngraecum ablum majus. It remained undiscovered until 1825 when Karl Ludwig Blume discovered the same species and gave it the name it is known by presently. This species is usually found in the eastern to southeastern regions of Asia. Plants in this genus are typically widespread in the areas of eastern Asia, such as China and Indonesia. This particular species wide-ranges from Indonesia to Australia. In fact, this species is one of Indonesia's national flowers (along with Jasminum sambac and Rafflesia arnoldii).Plants of this genus have a uniform structure that makes the identification easy for novice botanists. Phalaenopsis amabilis, like most of the other species in this genus, has a short stem. This is believed to be an adaptation to gain the light requirements needed to grow, according to Christenson. The rooting of P. amabilis is usually unbranched. The only times it would be branched are if the roots are damaged or if the individual has gotten old in age. The leaves ofP. amabilis vary from oblong to elliptic at the base and obtuse, minutely, at the tip or apex and measures at 50 × 10 cm. The moon orchid's flower is showy, membranous, white, the lip, (the unpared petals of an orchid) which is three-lobed, and the callus are a variety of yellow and red depending on the individual plant. It is able to bloom for a long period of time and can grow up to 10 cm in diameter and more.
Phalaenopsis amabilis reproduces sexually through pollination. This plant grows its flower to attract the pollinator. It is generally pollinated by large carpenter bees from the genus Xylcopa. For this particular species in the Phalaenopsis genus the pollination frequency and success rate is high (about 50%).
P. amabilis and the other species in the same genus grow naturally in three distinct habitats. The first is in seasonally dry areas, then seasonally cool areas and last constantly moist or humid areas (Christenson), developing adaptions for each habitat. For the seasonally dry habitats, Phalaenopsis species have an extreme adaptation in which it adopts deciduous habits, losing its leaves. They do this because in dry habitats, leaves are a serious liability when water isn't easily accessible. This adaptation typically occurs in species found outside the Himalayan region. For the habitats that are seasonally cool areas, the species found there are all deciduous or semi-deciduous in nature which means these plant have a strong dormant rest period. In this dormant period, the plants have protection from the cold due to the high carbon to nitrogen ratio and low water content on the leaf tissue. The constantly moist and humid habitats are the most common places that someone can find many of the Phalaenopsis species. In this habitat, the species grow in the canopy evergreen forests. Because they grow in the canopy, the species' adaptation is growing leathery leaves to prevent desiccation and so that the plants can tolerate higher light levels than other species.
According to Dressler, the plants of this family are thought to be closely related to plants that would have been classified in the Liliaceae or the Amaryllidaceae families.


Bunga Bangkai (Rafflesia arnoldii)
Rafflesia arnoldii is a member of the genus Rafflesia. It is noted for producing the largest individual flower on earth, and a strong odor of decaying flesh - the latter point earning it the nickname of "corpse flower". It occurs only in the rainforests of Sumatra and Borneo in the Indonesian Archipelago. Although there are some plants with larger flowering organs like the Titan Arum and Talipot palm, those are technically clusters of many flowers.
Several species of Rafflesia grow in the jungles of southeast Asia, including the Philippines. Many of them are threatened or endangered. The flower ofRafflesia arnoldii is the largest which attains a diameter of around one meter (3 ft) and can weigh up to 11 kilograms (24 lb). The largest recorded flower was measured at 1.04 metres on February 11, 2010, in Malaysia on the edge of the Cameron Highlands.It lives as a parasite on the Tetrastigma vine, which grows only in primary (undisturbed) rainforests. Rafflesia lacks any observable leaves, stems or even roots, yet is still considered a vascular plant. Similar to fungi, individuals grow as thread-like strands of tissue completely embedded within and in intimate contact with surrounding host cells from which nutrients and water are obtained. Perhaps the only part of Rafflesia that is identifiable as distinctly plant-like are the flowers; although, even these are unusual since they attain massive proportions, have a reddish-brown coloration and stink of rotting flesh, which is why it was nicknamed the "corpse flower". This scent attracts insects such as flies which then pollinate the rare plant. It is not to be confused with the Titan Arum, Amorphophallus titanum, which is also commonly referred to as the "corpse flower".

source:
http://news.bbc.co.uk/
http://www.plantlife.org.uk/
http://national-flowers.info/
http://www.theflowerexpert.com/
http://en.wikipedia.org/
http://wiyono4.blogspot.com/
http://mediaranahjaya.blogspot.com/

The Super Volcanoes in Indonesia

VEI (Volcanic Explosivity Index)

The Volcanic Explosivity Index (VEI) was devised by Chris Newhall 

of the U.S. Geological Survey and Steve Self at the University of

 Hawai?i in 1982 to provide a relative measure of the explosiveness 

of volcanic eruptions.

Volume of products, eruption cloud height, and qualitative observations

 (using terms ranging from "gentle" to "mega-colossal") are used to determine

 the explosivity value. The scale is open-ended with the largest volcanoes 

in history given magnitude 8. A value of 0 is given for non-explosive 

eruptions (less than 104 cubic metres of tephra ejected) with 8

 representing a mega-colossal explosive eruption that can eject 1012 

cubic metres of tephra and have a cloud column height of over 25 km (16 mi). 

Each interval on the scale represents a tenfold increase in observed eruption criteria.

Note that ash, volcanic bombs, and ignimbrite are all treated alike —

 this is due to taking into account the vesicularity (gas bubbling) of the 

volcanic products in question and the DRE (Dense-Rock Equivalent) is calculated

 to give the actual amount of magma erupted. One weakness of the VEI is

 that it does not take into account the magnitude of power output of an eruption. 

This, of course, is extremely difficult to detect with prehistoric or unobserved eruptions.

6. 1982 Eruption of Galunggung, (VEI 4)

Mount Galunggung (Indonesian: Gunung Galunggung, 

formerly spelled Galoen-gong) is an active stratovolcano in West Java, Indonesia.

The last major eruption on Galunggung was in 1982, which had a Volcanic 

Explosivity Index of 4 and killed 68 people. This eruption also brought

the dangers of volcanic ash to aviation to worldwide attention, after two Boeing 

747 passenger jets flying downwind of the eruption suffered temporary 

engine failures and damage to exterior surfaces, both planes being forced

 to make emergency landings at Jakarta.



one, a British Airways aircraft carrying 240 passengers, accidentally entered the

 ash cloud during night time in June 1982 150 km downwind of the volcano. 

All four engines failed and the aircraft descended for 16 minutes, losing 7500

metres of its 11500 meter altitude, until the crew managed to restart the engines.

The following month a Singapore Airlines aeroplane with 230 passengers aboard

 also inadvertently entered the cloud at night time, and three of its four engines stopped. 

The crew succeeded in restarting one of the engines after descending 2400 meters. 

Both aircraft suffered serious damage to their engines and exterior surfaces.


5. The 1963-64 Eruption of Mount Agung, (VEI 5)

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.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, 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.


4. 1883 Eruption of Krakatoa, (VEI 6)

Krakatoa (Indonesian: Krakatau), also spelled Cracatoa or Krakatau,

 is a volcanic island made of a'a lava in the Sunda Strait between

 the islands of Java and Sumatra in Indonesia. The name is used for

 the island group, the main island (also called Rakata), and the volcano as a whole.

The best-known eruption of Krakatua culminated in a series of massive 

explosions on August 26–27, 1883, which was among the

 most violent volcanic events in modern and recorded history.

With a Volcanic Explosivity Index (VEI) of 6, the eruption was 

equivalent to 200 megatons of TNT (840 PJ)—about 13,000 times the

 nuclear yield of the Little Boy bomb (13 to 16 kT) that devastated Hiroshima, 

Japan during World War II and four times the yield of the Tsar Bomba (50 MT), 

the largest nuclear device ever detonated



The 1883 eruption ejected approximately 21 cubic kilometres (5.0 cu mi)

 of rock, ash, and pumice.

The cataclysmic explosion was distinctly heard as far away as Perth in Western

 Australia, about 1,930 miles (3,110 km) away, and the island of Rodrigues

 near Mauritius, about 3,000 miles (5,000 km) away.

Near Krakatau, according to official records, 165 villages and towns were 

destroyed and 132 seriously damaged, at least 36,417 (official toll) people died, 

and many thousands were injured by the eruption, mostly from the tsunamis that

 followed the explosion. The eruption destroyed two-thirds of the island of Krakatoa.

Eruptions at the volcano since 1927 have built a new island in the same location, 

named Anak Krakatau (Indonesian: "Child of Krakatoa"). 

This island currently has a radius of roughly 2 kilometres (1.2 mi)

 and a high point around 300 metres (980 ft) above sea level, growing 5 metres 

(16 ft) each year.

3. Maninjau (280.000 BP), (VEI 7)

Lake Maninjau (Indonesian: Danau Maninjau, meaning overlook or 

observation in Minangkabau) is a caldera lake in West Sumatra, Indonesia. 

It is located 16 km to the west of Bukittinggi, at 0°19'S 100°12'E.

The Maninjau caldera was formed by a volcanic eruption estimated to have

 occurred around 52,000 years ago. Deposits from the eruption have been

 found in a radial distribution around Maninjau extending up to 50 km to

 the east, 75 km to the southeast, and west to the present coastline.

 The deposits are estimated to be distributed over 8500 km² andnhave a

 volume of 220–250 km³. The caldera has a length of 20 km and a width of 8 km.

2. 1815 Eruption of Tambora, (VEI 7)

Mount Tambora (or Tamboro) is an active stratovolcano, also known as

 a composite volcano, on the Sumbawa islands, Indonesia. Sumbawa is flanked 

both to the north and south by oceanic crust, and Tambora was formed by

 the active subduction zones beneath it. This raised Mount Tambora as high as 

4,300 m (14,100 ft), making it one of the tallest peaks in the Indonesian archipelago,

 and drained off a large magma chamber inside the mountain. It took decades to

 refill the magma chamber, its volcanic activity reaching its peak in April 1816.

Tambora erupted in 1816 with a rating of seven on the Volcanic Explosivity Index,

 making it the largest eruption since the Lake Taupo eruption in about 180 CE. 

The 1815 eruption of Tambora 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 an overestimate. The eruption created 

global climate anomalies; 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.

Using radiocarbon dating technique, it has been established that Mount 

Tambora had erupted three times before the 1815 eruption, but the magnitudes 

of these eruptions are unknown. Their estimated dates are 3910 BC ± 200 years, 

3050 BC and 740 CE ± 150 years. They were all explosive central vent eruptions

 with similar characteristics, except the lattermost eruption had no pyroclastic flows.

In 1812, Mount Tambora became highly active, with its eruptive peak in the 

catastrophic explosive event of April 1815. The magnitude was seven on the 

Volcanic Explosivity Index (VEI) scale, with a total tephra ejecta volume 

of 1.6 × 1011 cubic metres (160 cubic kilometers or 38 cubic miles). 

It was an explosive central vent eruption with pyroclastic flows and a caldera collapse, 

causing tsunamis and extensive land and property damage. It created a long-term 

effect on global climate. This activity ceased on 15 July 1815. Follow-up activity 

was recorded in August 1819 consisting of a small eruption (VEI = 2) with flames

 and rumbling aftershocks, and was considered to be part of the 1815 eruption. 

Around 1880 ± 30 years, Tambora went into eruption again, but only inside the caldera. 

It created small lava flows and lava dome extrusions. This eruption (VEI = 2) 

created the Doro Api Toi parasitic cone inside the caldera.

Mount Tambora is still active. Minor lava domes and flows have been extruded 

on the caldera floor during the 19th and 20th centuries. The last eruption

 was recorded in 1967. However, it was a very small,

 non-explosive eruption (VEI = 0).


1. The Toba Super Eruption, (VEI 8)

The Toba supereruption (Young Toba Tuff or simply YTT) occurred between 

69,000 and 77,000 years ago at Lake Toba (Sumatra, Indonesia), 

and it is recognized as one of Earth's largest known eruptions. 

The related catastrophe theory holds that this supervolcanic event plunged 

the planet into a 6 to 10 year volcanic winter, which resulted in the world's

 human population being reduced to 10,000 or even a mere 1,000 breeding pairs, 

creating a bottleneck in human evolution. Some researchers argue that the 

Toba eruption produced not only a catastrophic volcanic winter but also an 

additional 1,000 year cooling episode.

The Toba event is the most closely studied supereruption. In 1993, 

Michael R. Rampino of the New York University and Stephen Self of the 

University of Hawaii at Manoa first suggested a link between the eruption 

and a bottleneck in human evolution. The theory was then developed in 1998

 by Stanley H. Ambrose of the University of Illinois at Urbana-Champaign.

The Toba eruption or Toba event occurred at what is now Lake Toba about

 73,500 years (± 3,000 years) or 73,000 (± 4,000 years) ago. The Toba eruption

 was the latest of the three major eruptions which occurred at Toba in the last

 1 million years. The last eruption had an estimated Volcanic Explosivity Index

 of 8 (described as "mega-colossal"), or magnitude = M8; it thus made a sizeable 

contribution to the 100 X 30 km caldera complex. Dense-rock equivalent 

estimated of eruptive volume for the eruption vary between 2,000 km3 and

 3,000 km3, but the most frequently quoted DRE is ~2,800 km3 (7 X 10km18g) 

of erupted magma, of which 800 km3 was deposited as ash fall. It was two

 orders of magnitude greater in erupted mass than the largest volcanic eruption

 in historic times, in 1815 at Mount Tambora in Indonesia, which made 1816

 the "Year Without a Summer" in the northern hemisphere.

Although the eruption took place in Indonesia, it deposited an ash layer approximately

 15 centimetres thick over the entire Indian subcontinent. A blanket of 

volcanic ash was also deposited over the Indian Ocean, and the Arabian

 and South China Sea. Studies, based on deep-sea cores retrieved from

 the South China Sea, recently extended the known distribution of the eruption, and

 suggest that the ~2,800 km3 calculation of the eruption magnitude is a minimum

 value or even an under-estimate.

Source:

http://vulcan.wr.usgs.gov/

http://volcanoes.usgs.gov/

http://www.bbc.co.uk/

http://dsc.discovery.com/

http://volcano.si.edu/

http://geo.mtu.edu/

http://id.wikipedia.org/

http://kaskus.us/

http://www.tobavolcano.googlepages.com/

http://www.articlesextra.com/toba-supervolcano-indonesia.htm

http://mediaranahjaya.blogspot.com/

kisah kisah di 96

Kisah di 96

Pertama-tama nya sih di 96 baik baik aja , damai , tentram , dan nyaman , blom pada terlalu deket satu dengan yg lainnya.
Trus lama kelamaan jadi dah pada mulai deket , ampe sering gila-gilaan bareng.
Trus klo dipikir-pikir orang yg ska gila-gilaan bareng itu ternyata semuanya emg pada gila.
Tiap hari pasti ada aja bahan untuk ditertawakan , dan bahan tertawaan itu bukan hanya sekedar hal yg lucu tapi itu hal yg gila bgt. sampe akhirnya muncullah GANSTREESS , klo kata gue sih maksud dari kata itu adalah ,big>perkumpulan org gila semua , tapi klo kata yg lainnya mungkin berebeda.
oh iya ganstress itu pnya slogan dan dulu sih sering di pake tp krn dah ga lucu lagi jdi dah ga dipake dehhh.... kta slogannya sih” APA AJA BOLEH” dan yg pertama mencetuskannya adalah gue, gue sih dapet kata itu dari OPERA VAN JAVA . hehe =>

Ampe klo dipikir-pikir anak 96 tiada hari tanpa tertawa , klo misalnya bahan tertwaannya ga ada , pasti slalu ada ank lain yg bikin hal lucu.Bahkan ampe ada yg nyiksa temennya Cuma buat gila-gilaan bareng , dan gue sring jadi korban ank gila itu…
Huuu nyebelin….
Saat sedang disiksa gue ga bias berkutik yg , abisnya ank gila itu pada maen keroyokan , ya atu gue kaah lah…
Dan gue cma bsa teriak….
IBU…IBU….IBU….AHHHH… GUE BILANGIN EMAK GUE LO….IBU….
Dan mereka tetap nyiksa gue….
Uhhhhhh…..
Itu sih baru kisah gilanya.
Ada lagi ni kisah julukan dari ank 96 …
Ni ceritanya…


Kata2 julukan sih biasanya muncul karna peristiwa yg dialami ma seseorg , atow ga dari kelemahan org , atow ga dri nma ortu , atow ga dr hal yg dilakuin ama org.
• Nih misalnya kaya FA***L dia sering di panggil TUTS ama ank2 ,itu sih sebenernya nma ortunya sihh….
• Trus ada lagi , DH**A dia dipanggil DEDONK , itu sih panggilan dr kls 8 , lagi jga klo ga manggil gtu bngung , soalnya ada 2 dela di 96…
• Trus ada lagi si NA**A , di panggil IJAH krn dlu waktu kls tuju dia suka ngikutin gaya nya RUBEN ONSU…
• Trus Si ZI**I , di panggil KIWIL dari kls 8 karana rambutnya yg keriwil…
• Trus si E***A di panggil Mrs.JABS karna klo ngomongnya suka ngeJABS gtu deh…
• Trus gue , gue di panggil CIPONG , gara2 mata gue sipit trus gigi gue patah , mereka sih blgnyaompong , padahal kan ga ompong…
• Trus si Y**A , gue sih manggil dai GENDUT , abisnya dia mulai gendut padahal kan dlu kaga…
• Trus si D***A dipanggil DIDUL , untuk membedakan 2 dela yg ada di 96…
• Trus PIKUYANG , itu sih panggilan sayang dari S****A buat seseorg di 96…
• Trus si M*A di panggil MAMI krn dia cewe tertua yg ada di ganstress dan BAPA nya ada ank kls sebelah…
• Trus ada DINDUUND panggilan buat D**I…
• Trus ada ODOT panggilan sayang dari si GENDUT buat A**T…
• Trus ada AYAM panggilan buat S****I , dari nma ibunya yg di balik…
• Trus ada SINTONG panggilan sayang dr ODOT buat S****A…
• Trus DEWI PERSIK buat L****A panggilan sayang dari Y***S…
• Trus ada BANDOT buat N***L ….
Syapa lagi ya….????
Auh ahh elap…..
Itu julukan di 96 , ada lagi ni kisah cinta di 96…


Dari gila-gilaan bareng ternyata di 96 dah ada yg saling mengagumi satu sama lain , dan bermula dari kekaguman itulah bnyak murid 96 yg udah pada mulai PDKT alias pendekatan gtu deh…..
Nah…abis PDKT ini lah baru tuh bnyk ank 96 pada CINLOK.Abis cinlok trus pada jadian dan lumayan bnyk jga sih pasangan cinlok di 96 , klo diitung-itung ada…1…2…3…4…5…6…7…8…. Oh iya ada 6 pasangan.
Itu sih yg udah pada jadian blom lagi yg pada masi PDKT…
Bnyk jga sih yg saling suka di 96 , ampe akhirnya muncul TRIANGEL LOVE di 96 , mungkin krna cowoknyalebih dikit dr pada cewek kali ya…?
Jadinya satu co direbutin 2 cewe….
Di 96 tuh kira-kira ada….
5 cinta segitiga yg melibatkan 14 org….
Bnyak kan….???

Itu sih bru kisah cintanya…
Klo ini kisah perselisihan di 96…

96 yg tadinya damai tau-tau jd bnyk yg berntem , dan katanya bnyk yg ga suka gtu deh ama ganstreesss…
Tapi awal perselisihan itu gara2 ada cinta segitiga , kan jadinya cewe nya tuh pada berantem kan , gra2 cowonya mau di ambil ama cewe lain…
Sekarang sih masi pada ngumpet2 buat nyatain klo mereka benci , tpi KATANYA ntar ada yg bener-bener terang-terangan nyatain klo dia benci….
KATANYA sih ada yg gak suka gtu deh ama ganstresss , nyebelin bgt kan….???

Mungkin bru itu aja yg ada di kepala gue , ntar lagy ya ...???
gue mau mikir-mikir lgy tntang 96 yg seru dan gila...
Oh iya SORI ya klo ada yg ga suka ama catatn ini , gue cuma mau menceritakan tntng 96 , itu doank.,..
bwah-ha-ha-ha-ha-ha