11 April 2012
Berita Terkini Gempa Bumi Aceh Sumatera 11 April 2012
Description: Berita Terkini Update Perkembangan Gempa Di Sematera Aceh, Bengkulu dan sekitarnya | Rating: 4.5 | Informasi Gempa perkembangan berita terkini langsung dari lokasi tempat kejadian di Aceh, bengkulu dan sekitarnya wilayah Sumatera hati ini sangat mencekam. Pada postingan kali ini blog beritamandiri akan memposting tentang Berita Terkini Gempa Bumi Aceh Sumatera 11 April 2012. Masyarakat sekitar lokasi gempa sangat panik akan datangnya Tsunami. Dampak gempa besar berkekuatan antara 8,5-8,9 Skala Ricter (SR) di Simeulue Aceh sekitar pukul 15,38 WIB, membuat Bengkulu siaga terkait peluang tsunami.
Berita Terkini Gempa Bumi Aceh Sumatera 11 April 2012
Artikel Terkait: Berita Gempa Bumi Di Aceh
Berita Terkini Gempa Bumi Aceh Sumatera 11 April 2012, "Karena terlihat pada gambar berwarna kuning, sedangkan di Aceh warna merah," kata Kepala Badan Meteorologi Klimatologi dan Geofisika Bengkulu Dadang Permana, Rabu.
Ia menjelaskan, lokasi gempa besar itu berada 2,4 Lintang Utara (LU) dan 92.99 Bujur Timur (BT).
Kedalaman gempa itu sekitar 10 km dan jaraknya sekitar 346 km barat daya Simeulue, Aceh dan dirasakan di Sumatera Utara, Bengkulu, Sumbar dan Lampung. Khusus untuk Bengkulu getaran gempa itu cukup kuat dan warga berhamburan ke luar kantor dan rumah penduduk, namun tidak ada korban jiwa.
Nah, itulah seputar informasi Berita Terkini Gempa Bumi Aceh Sumatera 11 April 2012 dari beritamandiri (Berita Terbaru Indonesia). Semoga informasi tersebut bermanfaat buat anda dan para korban gempa di Aceh bisa tetap bersabar dan diberi ketabahan.
Sumber : Berita Mandiri.
Lhokseumawe
- Pasca terjadinya gempa yang berkekuatan 8,9 skala richter, seperti
menjadi pertanda besar bagi masyarakat Aceh khususnya. Betapa tidak,
Rabu kemarin (11/4), di langit Kota Lhokseumawe tiba-tiba muncul awan
putih yang mirip lafadz Allah. Munculnya lafadz Allah yang terbentuk
dari awan putih itu dipercayai sebagian orang sebagai pertanda besar
bagi rakyat Aceh.
Seperti yang diamati The Globe Journal kemarin, lafadz Allah yang terbentuk dari awan tersebut berlangsung sekitar sepuluh menit, dan kemudian hilang secara perlahan membentuk awan biasa. Hal tersebut membuat masyarakat di kota Lhokseumawe heboh dan langsung mengabadikan gambar tersebut dengan kamera digital serta ponsel.
Salah seorang warga lhokseumawe, Suryadi (24), menyebutkan, bahwa menurutnya baru kali ini hal seperti itu terjadi, muncul di langit Kota Lhokseumawe. “Ini pertanda besar bagi umat nabi Muhammad SAW. Kita hanya bisa berdoa dan berusaha,”ucapnya.
Pasca Gempa, Lafadz Allah 'Muncul' di Langit Lhokseumawe
Chairul Sya’ban | The Globe Journal
Kamis, 12 April 2012 12:22 WIB
Seperti yang diamati The Globe Journal kemarin, lafadz Allah yang terbentuk dari awan tersebut berlangsung sekitar sepuluh menit, dan kemudian hilang secara perlahan membentuk awan biasa. Hal tersebut membuat masyarakat di kota Lhokseumawe heboh dan langsung mengabadikan gambar tersebut dengan kamera digital serta ponsel.
Salah seorang warga lhokseumawe, Suryadi (24), menyebutkan, bahwa menurutnya baru kali ini hal seperti itu terjadi, muncul di langit Kota Lhokseumawe. “Ini pertanda besar bagi umat nabi Muhammad SAW. Kita hanya bisa berdoa dan berusaha,”ucapnya.
Sepanjang zona subduksi Pulau
Sumatera merupakan jalur gempa bumi yang paling banyak menyerap dan
mengeluarkan energi gempa bumi. Dalam sejarah, tercatat sudah banyak
kejadian gempa bumi dengan magnitudo di atas 8.0 (skala Richter dll)
[Natawidjaja, 2005; Newcomb and McCann, 1987]. Di Selatan Sumatera,
gempa besar pernah terjadi tahun 1833 (M8.9) dan tahun 1797 (M8.3-8.7).
Kedua gempa ini menghasilkan tsunami besar yang menghantam perairan
Sumatra Barat dan Bengkulu.
Di wilayah khatulistiwa, gempa besar terakhir terjadi tahun 1935
dengan kekuatan gempa M 7.7. Gempa ini menyebabkan kerusakan yang cukup
parah di Telo, kota Kecamatan di Kep. Batu dan juga wilayah sekitarnya.
Di beberapa tempat di Kep. Batu dilaporkan juga adanya kenaikan air laut
ketika gempa, namun tidak dilaporkan adanya kerusakan serius akibat
gelombang laut yang naik ini .Gempa dan tsunami besar juga pernah melanda wilayah Nias- Simelue pada tahun 1861 diperkirakan berkekuatan lebih dari 8.5 SR. Kemudian tahun 1907 terjadi kembali tsunami besar di wilayah Simelue dan Nias. Meskipun magnitudo gempa yang menyebabkan tsunami 1907 ini tidak terlalu besar (M7.6) namun tinggi tsunami yang terjadi di pantai barat dan Utara Simelue mencapai lebih dari 10 meter.
Bedasarkan catatan ,tinggi tsunami tahun 1907 dua kali lebih besar dari tsunami Aceh 2004 di wilayah Pulau Simelue. Peristiwa tsunami inilah yang konon melahirkan istilah “SMONG” atau bahasa lokal untuk tsunami. Orang-orang yang selamat saat bencana tsunami 1907 itu lantas menceritakan tragedi tersebut pada anak cucu mereka, turun temurun hingga kini. Inti nasehatnya kurang lebih adalah “apabila nanti air laut tiba-tiba surut sampai jauh ke tengah maka itulah tandanya smong akan datang, larilah cepat ke bukit, selamatkan jiwa dan tinggalkan saja harta benda”.
Gambar
1. Lukisan dari tsunami yang terjadi tahun 1861 di wilayah Sumatra
Utara, Nias, dan Simelue menggambarkan kedahsyatan dari tsunami
tersebut.
Gambar 2 : Peta Kejadian Gempa di Sumatera
Beberapa catatan dan Memoir tentang kejadian Gempa di Sumatera
Gempa tahun 1797 (10 Februari 10, pukul 10 malam)Naskah Asli dari catatan sejarah gempa 1797:
1.From [Wichmann, 1918b], pp. 74-75.
(English Translation by Jenny Briggs)
February
10, around 10 p.m. West coast of Sumatra. The first period of shaking
lasted one minute, after which a tidal wave immediately arose and forced
its way with such strength into the river at Padang that the town was
flooded.[2].
After this, the water withdrew so far that even the river bed was left
dry. This sequence was repeated three times. The village of Ajer [Air]
Manis, located on the beach, was flooded and several huts were swept
away. In Padang itself, crevices appeared that were 3-4 inches wide, but
these closed up again after further shaking occurred. However, cracks
formed in the walls of most of the buildings.
Throughout the entire night as well as throughout the whole of the next day,
February
11, the ground was moving. Every 15-20 minutes, severe shaking
occurred. For the duration of the entire following week, people felt the
ground trembling. However, the intervals of calm grew steadily longer.[3]
According
to J. Griffith’s reports, the earthquakes had spread over an area 2
degrees north and 2 degrees south of the equator. Moreover, the tidal
wave they generated also had effects on the Batu islands.[4].
J. Anderson mentioned, based on the report of S. C. Crooke, a severe
earthquake in the region of Djambi [Jambi], east Sumatra, “about 20
years prior to 1820” [5], and J. R. Logan thinks that it very possibly could have occurred in 1797 at the same time as the quakes in west Sumatra [6].
________
Footnotes:
1
“par les matières en fusion qu’on voyait bouilloner au fonds de son
cratère.” Deschamps. Precis sur l’ile de Java. Mem. de la Soc. roy.
d’Arras 3. 1820, p. 217.
2
.J. du Puy. Een paar aanteekenigen omtrent vuurbergen en aardbevingen
op Sumatra, Tidjschrift voor Neerl. 1845. 3, p 114. — Robert Mallet
(Fourth report on the Facts of Earthquakes. Report Brit. Assoc. Adv. of
Sci. 24. 1854. London 1855, p. 38) referred to the papers written by J.
Griffith in stating that this earthquake occurred on Feb. 20, but
Griffith’s reports certainly gave it no date. On Feb. 10, 1797, S. A.
Buddingh described an earth- and sea-quake at the Minnahassa on Celebes.
He reported himself that at Kema the tidal wave was so powerful that it
made the water in the rivers rise up, and that among others the village
of Ajer Madidi — halfway between Kema and Menado at an elevation of
232.3 m.– was flooded (Neederlandsch Oost-Indiё 2. Rotterdam 1860, p.
66.) In the entire report, not one word is true. Apparently he once
heard of the earthquake in Sumatra and, with the usual carelessness,
attributed it to northern Celebes.
3
.It was also reported that a ship was swept 3 miles toward land by the
tidal wave and that the wave caused 300 people to lose their lives
(Memoir of the Life and Public Services of Sir Thomas Stamford Raffles,
London 1830, p. 295).
4.
Description of a rare Species of Worm Shells, discovered at an Island
lying off the Northwest [sic!- A.W.- author] coast of Sumatra. Philos.
Transact. 96. London 1806, p. 269.
5. Mission to the East Coast of Sumatra in 1823. Edinburgh and London 1826, p. 402.
6. On the Local and Relative Geology of Singapore. Journ. Asiatic Soc. of Bengal. N.S. 16. Calcutta 1847, p. 549.
2.From [du Puy, 1845], pp 113-115. Translated by Maarten Schmidt, Caltech
Earthquakes are frequent on Sumatra, but they cause not much damage because of the low population.
The
strongest earthquake in the memory of the people in Padang, happened on
February 10, 1797 around 10 p.m. The moon which was full shone brightly
but darkened at the first quake and stayed so during the night – the
first shock lasted for about one minute – the waves of the sea ran with
fury up the river by which the whole place was flooded. Next, all the
water ran out the river, which was suddenly dry; this repeated itself
three times; the river banks were covered with fish; a sailing ship of
150 tons which was moored to a tree near the mouth of the river, broke
loose when the sea entered and was driven to behind the then-existing
fort, a distance of 3/4 Eng. miles; on the way the vessel hit a stone
house and two wooden ones which were demolished. Several smaller
vessels, which were moored in the river, were also dislodged and moved
off by the sea; some of these were later found behind the great market. A
storage building in front of the house of the Resident at the river
bank was lifted by the
rushing
waves and put down in the Chinese kampong – all of Air Manis, a seaside
village at the corner opposite the Padang harbor is flooded and many
houses flushed away – the next day one found several of the unfortunate
inhabitants dead on the tree branches, where they had climbed to save
themselves.
The
inhabitants of Padang left their houses and fled to the square outside
the city; they saw the ground break open at some places some 3-4 inches
wide, and then in further shaking close again. The earth was the whole
night, and the following day, in continuing movement; every15 to 20
minutes there was heavy quaking and it lasted a week that the ground was
shaking; the pauses became longer and longer. The walls of most of the
stone houses in Padang were torn, so that cases and furniture fell over
and much damage was suffered; in Padang itself only two people died.
A
less strong earthquake occurred in 1822 . . .[Shaking reports suggest
that this earthquake was caused by the Sumatran fault, far inland]
3.[du Puy, 1847], pp 55-56. Translated by Maarten Schmidt, Caltech
On
February 10, 1797, at 10 p.m. a heavy earthquake occurred which caused
the collapse of many houses. The shock was so strong that the ground
split open; further shocks were felt every half hour for five hours
during the night though they became weaker and weaker. At the time of
the first shock the sea came up three times, so high that it reached one
third of the height of the ‘Apenberg’, which did brake the force
somewhat, and all the ships outside the river were thrown onto dry land.
An English sailing ship of about 180-200 tons was found behind the Bird
Market the next morning. The sides of the river were covered with fish
and all seaside houses were flooded. Fortunately, this terror caused few
or no human casualties. Old people claimed that 40 years ago there had
been a yet stronger earthquake. [There was, in fact an earthquake in
1756 (Newcomb and McCann [1987]).]
Ringkasan:
Semua laporan dari gempa dan tsunami tahun 1797 terfokus pada akibat
tsunami di wilayah muara sungai sampai pelabuhan (Muaro Padang). Ini
tidak berarti bahwa limpasan tsunami hanya sangat terlihat di wilayah
ini, karena perumahan penduduk memang baru menempati wilayah ini pada
saat itu. Walaupun dilaporkan kerusakan di Padang cukup parah tapi yang
mati hanya dua orang.
Guncangan : Lama
guncangan yang terasa di Padang adalah satu menit. Laporan du Puy
[1845] mengindikasikan bahwa gempa ini adalah yang terkuatdalam ingatan
penduduk Padang waktu itu. Namun pernyataan ini berlawanan dengan
laporan du Puy tahun 1847 yang mnyebutkan bahwa ada gempa yang lebih
kuat yang terjadi 40 tahun sebelumnya (~1757). Banyak rumah yang ambruk
ketika gempa. Di tanah terbanyak banyak rekahan dengan bukaan 3 – 4
inci.
Tsunami :
Beberapa orang yang berusaha memanjat pohon untuk menghindari tsunami
di Air Manis keesokan harinya ditemukan sudah mati di atas pohon.
Seluruh kota terendam bah tsunami dan beberapa rumah dilaporkan hanyut
terbawa gelombang. Di Padang dilaporkan tsunaminya juga menggenangi
”seluruh” kota. Orang melaporkan ada 3-4 kali gelombang ”pasang-surut”
di pelabuhan. Satu laporan menyatakan bahwa tsunami naik sampai
sepertiga Bukit atau Semenanjung Apenberg (Gunung Padang) (Gbr 2.3) yang
tinggi totalnya 104 m. Artinya tinggi tsunami mencapai 30 meteran.
Laporan itu juga menyebutkan bahwa Bukit appenberg tersebut memecahkan
gelombang tsunami. Laporan lain menyebutkan bahwa ketika tsunami tinggi
air laut adalah sekitar 50 kaki di atas normal. Di Padang, gelombang
”pasang-surut” tsunami membuat dasar sungai terlihat kering dan
meninggalkan banyak ikan mati di atasnya. Semua perahu di sungai menjadi
berada di atas tanah kering. Ada kapal besi dari Inggris seberat 150
-200 ton yang ditambatkan ke sebuah pohon di dekat muara sungai terbawa
gelombang tsunami sampai 0.75 mil ke arah hulu dan kemudian terdampar di
daerah Pasar Burung. Kapal ini merusakkan beberapa rumah takkala saat
terhanyut. Semua rumah di tepi laut dikabarkan tenggelam oleh air bah.
Interpretasi:
Di Air Manis, di sebuah kampong kecil di tepi pantai sebelah baratnya
bukit Apenberg (Gunung Padang), tinggi tsunami cukup untuk
menenggelamkan orang yang berusaha memanjat pohon-pohon untuk
menghindar. Pohon-pohon ini kemungkinan sekitar 4-5 meter untuk dapat
menahan beban rata-rata orang dewasa. Kemudian dari fakta bahwa glombang
tsunami bisa membawa kapal besi Inggris seberat 150-200 ton artinya
bahwa tinggi tsunami (=”flow depth”) paling tidak 5 meteran mengingat
tinggi pinggiran sungai adalah sekitar 2 meter dan ”draft” bawah kapal
mungkin sekitar 3 meteran. Jadi dari dua catatan kejadian ini dapat
dapat disimpulkan bahwa tinggi gelombang tsunami adalah sekitar 5
meteran. Ini adalah perkiraan yang cukup konservatif dibandingkan dengan
laporan yang menyebutkan bahwa tinggi gelombang adalah sekitar 30 meter
di tepi bukit Apenberg dan sekitar 50 kaki (15 m) ditempat lainnya di
sepanjang pantai. Kami sangat meragukan laporan ini, karena kalau benar
seharusnya
tsunami sebesar ini menghancurkan seluruh perumahan penduduk di Padang
dan menyebabkan kemaian yang lebih banyak lagi. Kami memperkirakan bahwa
tinggi maksimum gelombang tsunami-nya kurang lebih setinggi 5 sampai 10
meteran.
Gempa tahun 1833 (24 November, pukul 8 malam) Catatan Asli sejarah gempa tahun 1833:
1.From [Wichmann, 1918b], pp 94-97.
(Translated by Jenny Briggs)
January
28, a few minutes after 12 noon. Batavia. Earthquakes. The shocks were
repeated, gaining in severity. The last one was so strong that several
houses were damaged and even the old Lutheran church developed cracks.
January
29, noon. Tjiwidei. District of Tjisondari, Division of Bandung,
Preanger regency, Java. Severe quakes, one of which was followed by
rumblings from the earth that lasted one minute.
November 24, around 8:30 p.m. Sumatra. Severe earthquake, that was felt in Singapore and even in Java.
In
Bengkulen [Bengkulu], on the west coast of Sumatra, there were severe
quakes, the first of which lasted 5 minutes4 and caused damage and even
destruction of buildings. The tidal wave which crashed into the coast
destroyed the harbor dam and all houses nearby. Two schooners, along
with several smaller crafts, were flung onto the land.
Padang. Severe quakes, lasting 3 minutes, which recurred over the following days.
Direction
SSW-NNE. Apart from the damage to buildings, cracks also appeared in
the earth, from which water and “sulfurous steam” arose. Each quake was
accompanied by a subterranean crashing noise. A tidal wave that broke
here did considerable damage.
Indrapura
and Pulu Tjingko [Cinco island]. Severe shaking. The damage caused here
by the tidal wave was significant, and people also lost their lives.
From the Gunung Singalang (volcano) people heard a loud boom, which, as
at the Merapi volcano (which was initially blamed for the explosion),
was followed by an eruption.
Priaman.
The most intense quakes. Cracks of two or more feet in breadth appeared
in the earth. The sea drew back and then returned in the form of a
powerful tidal wave, which tore numerous ships from their anchors. The
shaking continued for many days.
Province
of Rau, Division of Lubuk Sikaping. The Amerongen Fort was forcibly
attacked by rebellious natives during the time of the earthquake itself;
they interpreted the shaking as a good sign.
Palembang.
The first quake, noticed at 8:30 p.m., was followed by 6 others.
Direction S-N. Buildings developed cracks and several huts collapsed.
The
Ajer [Air] Lang river, whose source was at the volcano Bukit Kaba, had
run dry 3 years previously when an earthquake was followed by a
landslide that created a dam and a lake. During the earthquake of
November 24, however, this dam was destroyed again, which emptied the
lake. In their stormy course, the tumbling waters either partly or
completely destroyed the village of Kapala Tjurk on Ajer Lang, as well
as the more distant villages on Ajer Kling: Udjan Panas, Lubuk Talang,
Ajer Apo, Lubuk Tandjung, Tabah, Njambikei and Grung Agung.
Singapore.
At 8:35 p.m. a weak shock was felt, followed by a shaking of the ground
that lasted for a minute or perhaps somewhat longer. The vibrations
experienced in the encampment of Glam were stronger than those in the
town itself. In the report it was noted that this was the first
earthquake in Singapore since its occupation by the English (1819).
On Java, the quake was also weak; reports simply noted this fact.
On
the high seas, the quake was also experienced. The ship “Mercurius”,
which at the time was above the Pageh [Pagai] Islands on the west coast
of Sumatra, was shaken by heavy quakes.
August 26. The island Ramiri on the coast of Arakan, Birma.
During the earthquake, people observing the mud volcano from Kyauk Phyu, [a
town/place- J.B.] which lay off its northern peak, saw flames and steam rising several hundred feet above the volcano’s summit.
November
25, 7 a.m. Singapore. A quake, followed by a second one at 5 a.m. [sic-
J.B. This may be an error in the original that should be p.m.?]
Direction E-W.12
Pulu Painang (Penang). Earthquake.
2. From [du Puy, 1847], pp 156-158. Translated by Maarten Schmitt, Caltech
To the editors of the Journal of the Dutch (East) Indies
A friend and lover of the sciences has enabled me to communicate the following
observation of a major earthquake, falling in the time interval between the observations of Mr. du Puij and mine.
Dr. A.F.W. Stumpff
On
November 24, 1833, around 8 p.m. oscillating earthquake shocks were
felt in Padang, on the W. coast of Sumatra, which at first were not
thought to be serious; soon, the shocks were so violent that all went
outside, fearing to be buried under the wiggling buidings. Outside, with
the earth shaking under one’s feet, one saw in a bright moon buildings
and trees in hefty motion, the ground splitting with water bubbling up
with major force, while the river was threatening to overflow. The sea
was extremely active, one was fearful of it rushing in causing
destruction as had happened in a similar natural event late in the last
century. This situation
lasted somewhat over three minutes.
The entire population of Padang was afoot, those living along the river trying to reach higher lying areas of the city.
During
the months of August, September and October one had observed extreme
heat and humidity; the day of November 24 characterized itself by a deep
silence in all of nature, that had not then been noticed, however; the
terrible motion that followed was not without consequnces. In the
houses, everything was overthrown, especially the stone houses were
subject to great destruction through the tearing and separating of walls
and the collapse of stone pillars. At sea there was also much
commotion. Ships in the port of Padang moved on their anchors, some of
which were lost.
An underground noise preceded the motion, after which mud and sulfur-like fumes rose from the split ground.
Several
hours before the first shock, one had seen along the beach a
surprisingly large amount of fish; the following day many dead fish were
observed at the same location.
It
was noteworthy that the volcano Merapi in Agam was not particularly
active during this terrifying event; it had early thrown out much fire
and ash but during the general upheaval the mountain was quiet; only
after the first motion one had observed a terrible bang, which some here
in Padang also believed to have heard.
Elsewhere,
local circumstances seem to have offered more resistance to the
destructive force. At Poelo Cinco [Cinco island], the sea rushed in and
carried off several houses and also people.
At
Indrapoera there was also some destruction caused by the sea and a few
people died. At Benkoelen [Bengkulu], all buildings had much damage, so
much so that the tower and the fort had to be taken down; the pier with
the storage building and the customs office were wiped out, two
government and several other ships were deposited on the beach, however
no lives were lost there. Shocks were felt far into the ocean. The
captain of the ‘Mercury’ tells that near the Pagai islands, hundreds of
miles offshore, he experienced the shocks as if he had hit cliffs.
Experts are assuming that this earthquake moved from SSW to NNE. The first and
strongest
motion was simultaneous with spring tide, three days before Full moon.
The atmosphere seems to have been little affected and weather stations
saw no change. The same night and following days were characterized by
shocks ofvarying strengths until the end of November.
3.From [Verkerk, 1870], pp 314-328. Translated by Maarten Schmidt, Caltech
[Summary:
The article describes the first part of an ascent of themost active
volcano in the Palembang Highlands, the Holy Mountain]
Kabaa. On the way, the author descibes his stay in Apoor, where he is hosted by the old man Tjermin.]
About
25 years ago, the region east of Kaaba was subject to an upheaval, so
terrible in its consequences, that it has erased people’s memory of all
previous disasters.
Some
three years earlier, one of the streams originating on the Kaaba, the
Ajer Lang, had suddenly dried up. An earthquake close to its origin had
made a dam over the stream bed: the water could not escape and created a
lake in a nearby valley. The damage caused by the lack of water along
the Lang was repaired and forgotten, and the fear of disaster had
subsided among the people – when suddenly terror struck. This time it
happened in the middle of the night. Awakened by the hefty shocks of the
booming earth, which was staggering like a horse driven by its rider,
they rushed outside. From the steep, nearly verical, side of the Lang,
which near the village Kapala Tjoeroek is about 100-200 feet high, and
where the bamboo huts cling to the side like bird nests, they looked
down into the river; but who can descibe their terror when they saw in
the bright lightning flashes, there in the depths where hours earlier
there had been nothing but a dry rocky bottom, a screaming and boiling
sea that rose up from the abyss as if to swallow the mountain.
The lake had broken through its dam and rushed as if in one jump into the Kapala
Tjoerek
bed! – The hapless! could hardly believe their eyes. As in a terrible
dream, swaying between doubt and fear, they kept staring, and even
though the danger increased all the time, none were thinking about
saving themselves. None of them would escape. Not even the few who, not
mesmerized by fear, ran up the mountainside. The faster and faster
rising flood overtook them all. The disaster took more than 120 lives.
Tjermin’s wife was also killed. A number of villages were totally or
partly destroyed. Except for Kapala Tjoeroek at the Lang, the following
places on the Klingi (into which the Lang empties): Oedjan Panas, Loeboe
Talang, Ajer Apo, Loeboe Tandjoeng, Tabah, Njambikei and Goeroeng
Agoeng. After two days the Lang went down to its present day level. It
was finally noted that three elephants were moved along in the stream.
4.From: Jeffrey Hadler, U California, Berkeley, email communication 21 April 2005 ; …
I’ve been writing to fellow historians and Anthony Reid has this 1833
anecdote: ‘I was fascinated by 1833, and share your wonderment that we
have not heard more about it in the literature. I looked up the book I
happen to have of Henry Lyman: The Martyr of Sumatra, since he was in
Padang about that time. It turns out he arrived Padang only early 1834,
but noted of Sunday 23rd Feb 1834 that he preached on board a ship, the
Eugene, and “Heard of an earthquake at Padang whch very much damaged the
hill; opened the river so as to make it dry, and filled it with fish
not known before. It also drove on this coast a large shoal of fish,
never before seen here, something like alewives.” (pp.289-90).’.
5. From [Boelhouwer, 1841], pp 175-176. Translated by Maarten Schmidt, Caltech
I
should not forget to mention an earthquake that we felt at the end of
November. In the evening there were very heavy shocks, such that all of
us feared for our lives and none, not even the oldest natives, could
recall something like this. It was impossible for me and anybody else to
stay in the house, and we could not even keep standing; all of nature
seemed to be in turmoil, everything was shaking and was falling apart;
nothing that had been on tables or in cabinets stayed there; the earth
opened up at various places, creating fissures two or more feet wide.
The sea retreated with furious power a long way, from which she came
back in with double fury; none of the ships off Priaman stayed anchored,
all were torn away and we found them the next morning at large
distances, spread left and right. For several days there was shaking,
though less. In Padang, several stone buildings, including the church,
suffered much damage; the church could not be used any more, and on my
journey to Padang I saw terrible grooves (rills) on the beach. At
Benkoelen, as we learned later, the entire harbor head as well as the
tax office for Import and Export were destroyed.
J.C. Boelhauwer seorang komandan militer Belanda di Pariaman
(J.C. Boelhouwer, Herinneringen van mijn verblijf op Sumatra Westkust gedurende jaren 1831-1834 (Kenangan-kenangan di Sumatra Barat dalam tahun-tahun 1831-1834)) (1841)
…di
akhir November 1833, terjadi gempa besar yang menggoncang daerah
Pariaman dan Padang. “Pada malam harinya kami mengalami ketakutan hebat
yang membuat kami khawatir akan hidup kami. Bahkan orang pribumi yang
paling tua pun tidak pernah mengingat hal seperti itu pernah terjadi”,
demikian tulis J.C. Boelhauwer , “Saya dan orang lain tidak dapat
tinggal lebih lama di dalam rumah dan bahkan kami tidak dapat berdiri di
halaman. Seluruh alam terasa dalam huru-hara, segala sesuatunya
terguncang dan jatuh berpecahan. Tidak ada satupun di atas meja atau
kursi yang tetap tinggal pada tempatnya. Di beberapa tempat tanah
terbelah selebar dua kaki atau lebih. Laut bergolak dan terus bergolak
makin dahsyat. Tidak ada perahu di pelabuhan Pariaman yang tetap
tertambat di dermaga. Semuanya terhanyut jauh dan esok paginya kami
menemukan perahu-perahu itu terpencar dimana-mana. Beberapa hari
kemudian, masih terasa beberapa gempa lagi, walau dengan goncangan yang
lebih kecil. Di Padang sejumlah rumah batu, termasuk gereja, rusak
parah. Gereja malah tak bisa dipakai lagi. Dalam perjalanan saya ke
Padang, saya menemukan beberapa parit perlindungan yang rusak berat di
pantai”..
“Di Bengkulu, sebagaimana kami dengar kemudian, seluruh dermaga hancur, kecuali kantor bea cukai.”
Tampaknya
gempa yang terjadi pada waktu itu, yang juga menimbulkan tsunami, tidak
kurang dahsyatnya dari yang terjadi minggu lalu. Sebelum itu, waktu
Boelhauwer belum lama berada di Sumatra Barat, telah terjadi pula gempa.
“Pada
suatu malam ketika saya bertamu [di rumah seorang pejabat Belanda di
Padang—Suryadi] terasalah gempa yang menyebabkan seorang nona yang duduk
di atas bangku-bangku akan meluncur ke bahagian lain seandainya tidak
lekas dipegang oleh beberapa pemuda. Ada yang cepat memegang lampu dan
ada yang memegang gelas-gelas di atas meja. Gempa itu berulang beberapa
kali. Itulah gempa yang pertama kali saya alami, seolah-olah kita
dibuaikan. Kata orang yang telah mengalami gempa, gempa kali ini adalah
musuh yang kuat selama saya berada di Sumatra”, demikian tulis Boelhouwer (ibid.).
6. From [Mueller and Horner, 1855], pp 25-27. Translated by Maarten Schmidt, Caltech
Earthquakes
are often felt at Padang, but rarely of such intensity that they
endanger inhabitants. The most powerful earthquake since many years
occurred on November 24, 1833, just after 8 p.m., for about 2 minutes.
The air was damp, quiet and humid, in moonlight. The oscillating
movement of the earth, together with underground shocks and a rattling
sound that clearly came from the S.E., made everybody rush out of their
houses and created fear in all. One heard everywhere a hard stomping of
“rijstblokken” [rice blocks?] and people yelling. Along the river
fissures had opened here and there, which then closed again. The sea had
repeatedly run up the sloping beach, up to 10 to 12 “voet” [Dutch foot,
approximately equal to an English foot] high. All wooden houses creaked
and shook enormously; but the stone houses fared worse, with damaged
walls, some fell over, and some roofs that collapsed. In some houses,
furniture had been thrown from one corner to the other. There was
considerable damage but few accidents. Only one native and two cows were
lost. Curious is the large area over which the earthquake was noticed.
The shaking was felt in Natal, Tanapoeli, Singapore, on the N. coast of
Java, in the Lampongs, at Palembang and on Benkoelen [Bengkulu]: so over
an area of at least 150,000 sq. miles, or about as large as France. At
Benkoelen, the shocks wereheavier with more damage to the beautiful
stone buildings, than at Padang. At the beach near Indrapoera the sudden
rise in the ocean, which rolled in terrible waves over the low country
side, a small village was entirely destroyed where a woman with her
child disappeared in the water, while some people found refuge in trees
where they stayed until the next morning. Also in parts of inner Sumatra
the shocks were extremely violent, among others in the region Rau where
just then the Dutch fort Anerongen was besieged by thousands of
mutineers who considered this natural phenomenon a favorable sign for
their side. The two volcanoes Merapi, in Agam and Korintji [Kerinci],
gave at that time some indication of increased activity, though not such
that their natural chimneys seemed to contribute to a diminishing and
calming down of the underground explosive forces. This was provided by
the small volcano Kaba, located in the hinterland of Palembang, between
the high volcanoes Dempo and Merapi of Korintji, closer to the Dempo.
From the capital Benkoelen the Goenong Kaba lies E.N.E. at 40 geogr.
Minutes distance; from Palembang about 2 degress W.S.W. This volcano is
only 1500-1800 “voet” (feet) high and has several peaks, among which
besides the smoking crater there used to be a small lake, called Talaga
Kitjil, probably an inactive caldera filled with rain water. During the
earthquake, the Goenoeng Kaba had a terrible eruption, on which occasion
the Talaga Kitjil emptied over the low country to the S.E.; a flood
that in its path destroyed and swept off everything, jammed up several
rivers and caused major destruction in the districts Sindang-Klingi and
Sindang-balita. A small village in a valley close to the foot of the
mountain, was inundated to a height of 20 feet, at the end leaving a mud
layer of 7 feet high, together with uprooted trees, rocks, and the
bodies of 36 victims as well as many dead animals. In the two districts
there were in total 90 casualties. The water in the river Moesi, near
Palembang, was unfit to drink for several weeks due to sulfuric acid.
During the night of 24-25th November 1833, 11 more earthquakes were felt
and they continued with decreasing strength until the end of the year.
The central point of the forces working inside the earth were clearer in
the neighborhood of Goenong Kaba, where the shocks and loud underground
noises were far and above the heaviest.
7. EARTHQUAKE IN JAVA. The Hague, June 29
The
accounts received from Java, to the 26th of February, contain nothing
of general interest: but one of the papers gives some particulars of the
earthquake in the night of the 24th of November last. “This earthquke
which was flet in Java and elsewhere, especially in Sumatra, is ascibed
in a report from Palambang to an eruption of the Volcano Bocker(?) Kaba,
in Palambang. Besides the damage done by repeated shocks of the
earthquake, the effects of an inundation coming from that mountain were
most distressing. Between the two principal peaks of the mountain there
was a lake, called Telaga Ketjtel (?), which, in consequence of the
shocks of the earthquake, inundated the neighbouring districts. The
inundation was increased by the overflowing of the river Ager
Dinglen(?), the channel of which was choked up by masses of earth and
trunks of trees. The hamlet of Talbang Ager Lang was covered with water
to the depth of 21 feet, and after the inundation there remained a bed
of mud seven feet deep. Thirty-six inhabitants of the hamlet perished.
The total number of victims in the districts was 90. Mount Kaba is 50
leagues from Palambang, and yet the water of the great river Moessie (?)
[Musi] was not fit to drink for several weeks. An account from Kodal
states that on the 2nd of February, during a torrent of rain, part of
the mountain of Telo Mejo (?), in the district of Ngassinan(?), on the
frontiers of Ansbarawa, had sunk down, by which 12 habitations were
buried, and 37 persons lost their lives.
8.
Excerpt from letter by Lionel Jackson, Donald Forbes, John Shaw, Vaughn
Barrie, GSC Seychelles Tsunami Expedition, Canada, to Irwin Itzkovitch,
Canada,7 February 2005
It
is our pleasure to inform you that the GSC Indian Ocean Tsunami
Expedition to the Republic of Seychelles (RS) returned to Canada this
past weekend. We consider our expedition, which was to investigate the
tsunami that struck that island archipelago nation on 26 December 2004,
an unqualified success.
…
We arrived in RS the morning of 22 January and departed the morning of 3
February. We investigated the tsunami and its impact on the two largest
granitic islands, Mahé and Praslin, where most of the population of
about 80,000 reside.
The
tsunami resulted in significant property damage but only two fatalities
in RS. Two factors worked in RS’s favor: the tsunami struck during low
tide and it was a Sunday so most businesses in the commercial and
industrial areas of Victoria, the capital, were closed. These areas were
extensively flooded and boats and debris were driven ashore.
Furthermore, children were not in school. Had the tsunami struck at high
tide on a normal working day, the death toll could have been scores or
hundreds.
Lastly,
we were able to obtain tidal data recorded during the Krakatoa tsunami
of 1883 from the RS National Archives in Victoria and from the 1888
Royal Society report that we examined in the British Library in London.
This data set can be compared with the water level records from the 2004
tsunami, which appears to have been larger and more damaging that the
Krakatoa event. The archival investigation also uncovered evidence of
another tsunami that struck the islands ca. 1833 and may have been
comparable to the 2004 event.
9. From the National Archives, Seychelles, via Phil Cummins, Australia, via Lionel Jackson, Canada.
F/2.14 v. 17, item 44. pp 115-116.
Extract
from the Mercantile Record and Commercial Gazette, 5 October 1883,
which reports extensively on the tsunamis in the Seychelles produced by
the eruption of Krakatau in 1883.
… The following report has been kindly forwarded by Mr. H.W. Estridge, Collector of Customs at Mahe: …
I may remark that Mr. Beauchamp D’Offay, aged 67, told me that the same thing
happened 50 years ago. He recollects it well. The tide then went into the houses, was knee deep, and came in with a roar.
Ringkasan:
Guncangan gempa terasa sampai 5 menit di Bengkulu dan sekitar 3 menit
di Padang. Guncangan terasa sampai sejauh Singapura dan Jawa. Terjadi
tsunami besar yang merusakkan wilayah Bengkulu, Pulau Cinco, Indrapura,
Padang, dan Pariaman. Laporan menyebutkan tidak ada korban mati di
Bengkulu dan hanya satu yang mati di Padang.
Guncangan:
Guncangan sangat kuat di wilayah sepanjang pantai dari Bengkulu sampai
Pariaman dan juga di Pulau-pulau Pagai. Di Pariaman goncangan demikian
kuat sehingga tidak ada orang yang bisa berdiri. Kerusakan besar terjadi
di Padang dan Bengkulu, tapi yang lebih parah adalah di Bengkulu,
dimana seluruh struktur bangunan rusak berat. Benteng dan menara harus
di hancurkan total. Di Padang, rumah-rumah kayu tidak rusak tapi banyak
rumah dari batu tembok rusak parah. Di bagian Sumatra bagian timur
kerusakan bangunan dilaporkan sampai ke Kota Palembang. Rekahan tanah
selebar 2 kaki terjadi di Pariaman, dan juga banyak retakan-retakan
tanah di sepanjang pantai antara Pariaman dan Padang dan di pinggiran
sungai di Padang.
Tsunami:
Tsunami. Di Padang banyak kapal yang terbawa hanyut bersama jangkar
yang ditambatkan, dan sebagian hilang. Di pantai hempasan tsunami
mencapai ketinggian 3-4 meter. Peta kuno Kota Padang pada tahun 1828
memperlihatkan perumahan yang masih sedikit di sepanjang pantai, dan
pusat kota masih berda di wilayah bagian Utara sungai, sampai sekitar 1
kilometer ke arah darat. Dermaga dan bangunan pelabuhan di Bengkulu
tersapu ludes oleh tsunami, dan beberapa kapal terhempas ke darat. Di
Pariaman, dilaporkan tsunami didahului oleh surutnya air laut. Gelombang
menghempaskan kapal-kapal dari tempat tambatnya ke samping kiri dan
kanan. Di Pulau Cinco, gelombang tsunami menyapu ke darat menyapu
beberapa rumah dan orang. Di Indrapura, di utara Kota Bengkulu, tsunami
yang dahsyat menerjang daratan membanjari daratan rendah. Ada satu
kampung yang tersapu bersih oleh tsunami. Satu orang ibu beserta anaknya
terbawa tsunami dan hilang, tapi banyak orang yang bisa menyelamatkan
diri dengan memanjat pohon dan kemudian menunggu sampai pagi. Tsunami
yang sampai di Pulau Seychelles yang berada sekitar 5000 km dari pantai
barat Sumatra di lautan Hindia tingginya sama seperti yang terjadi pada
waktu tsunami Aceh-Andaman tahun 2004.
Gejala gunung api : Dua
gunung api, Marapi dan Kerinci, memperlihatkan kenikan aktifitas
setelah gempa. Runtuhnya dam alam di puncak Gunung Kaba menyebabkan
banjir di lembah-lembah di lereng sebelah tenggaranya. Banjir bandang
ini menyebabkan hilangnya 90 orang penduduk. Satu kampung tenggelam oleh
banjir yang dalamnya sampai 20 kaki (~6 meter) dan kemudian
meninggalkan timbunan Lumpur sedlam 7 kaki (2 meter lebih).
Interpretasi
: Lamanya goncangan dari gempa dan luas cakupan serta hebatnya
kerusakan yang ditimbulkan mengindikasikan bahwa sumber gempanya sangat
besar. Fakta bahwa kerusakan lebih parah terjadi di Bengkulu daripada di
Padang adalah indikasi yang kuat bahwa sumber gempanya lebih dekat ke
Bengkulu, artinya berda di bawah Kep.Pagai tapi tidak sampai ke Siberut
(pulau yang berhadapan dengan Padang). Kerusakan akibat tsunami juga
dilaporkan lebih besar/parah yang terjadi di Bengkulu – Indrapura
daripada di Padang. Memang dilaporkan bahwa kapal-kapal di Pariaman
terlepas dari tambatannya, tapi deskripsinya menunjukan bahwa gelombang
airlaut tidak sampai melewati dam alam di pinggiran sungai seperti
halnya tsunami yang terjadi pada tahun 1797.
Meskipun
demikian catatan sejarah menunjukkan bahwa gelombang laut mencapai
ketinggian 3-4 meter di pantai Padang, yang tentunya cukup untuk menyapu
wilayah pantai sampai beberapa ratus meter ke darat. Tapi kelihatannya
tidak melanda banyak perumahan yang masih jarang seperti terlihat di
peta tahun 1828
Gambar.
3. Peta Kota Padang dari tahun 1781 – 2005 digambar kembali dari arsip
peta kuno [diambil dari Natawidjaja et al., 2006].
Catatan seorang pedagang asal Pariaman,Sumatera Barat
Muhammad Saleh Datuak Urang Kayo Basa, Riwajat hidoep dan perasaian saja (huruf Jawi) (1914).
Pedagang
terkaya Pariaman pada abad ke-19 yang kapal-kapal dagangnya berlayar
sampai ke Susoh, dalam momoirnya, menulis bahwa di bulan Februari 1861
terjadi lagi gempa hebat, dengan episentrum di sekitar pulau Nias, yang
juga menimbulkan tsunami: “…pasar Singkil tenggelam, terbenam karena
gelora naik yang disertai dengan gempa bumi. Di laut dekat Tarumun
[Trumon, Aceh Barat—Suryadi] Gosong Djawi-djawi…[yang] penuh ditanami
orang nyiur kini hilang lindang dengan tidak meninggalkan kesan”,
demikian ditulis oleh . Salleh menceritakan bahwa banyak orang di
Singkil dan daerah sekitarnya mengungsi ke Ujung Bawang. Makam Syekh
Daud Sunur, pengarang SyairSunur yang terkenal, di dekat pasar Singkil juga habis disapu tsunami.
Dari
catatan sejarah dan folklor tersebut menjadi bukti bahwa Pulau Sumatera
memang sejak zaman kuno sudah menjadi ‘langganan’ gempa.
Sumber tulisan :
- Gempabumi dan Tsunami di Sumatra dan Upaya Untuk Mengembangkan Lingkungan Hidup Yang Aman Dari Bencana Alam ; Danny Hilman Natawidjaja
- Hidup Di Negeri ‘Langganan’ Gempa; DR.Suryadi,Peneliti Sejarah Leiden University
- Sumber : www.gempapadang.wordpress.com
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