Billitonites, Satam Stone, Batu Satam, tektite, Billiton, Belitung, Island, Formation

BILLITONITE / SATAM STONE FORMATION

Billitonites are basically the same as Philippinites. They are slightly more distal than most Philippinites (except for those from Mindanao). They are also heavily etched due to the acidic waters in Belitung. There are some subtle differences between the two and we'll examine them here.

 

Summary of Billitonite Formation:

Ringkasan Terbentuknya Batu Satam: 

Thanks to Arum Suryanti for providing the translation! You can translate more of this website using Google Translate

 

1) Around 780,000 years ago a large asteroid impacts in Indochina (possibly in the Bay of Tonkin). The asteroid travelled from a NNW to SSE direction and impacted at a low angle.

1) Sekitar 780.000 tahun yang lalu sebuah asteroid yang besar menabrak bumi di Laut Cina Selatan (kemungkinan di Teluk Tonkin). Asteroid ini bergerak dari barat laut ke tenggara dan menabrak bumi dengan sudut tabrakan yang kecil.

 

 

2) In the early stages of impact, the kinetic energy of the impacting asteroid melts and passes momentum to surface layers of terrestrial rock (such as sands and shales) at the impact site.

2) Pada tahap awal dari tabrakan, energi kinetis dari asteroid yang menabrak bumi ini melelehkan dan menghantarkan momentum kepada lapisan atas dari batuan di permukaan bumi (seperti pasir dan lumpur) di daerah tabrakan.

  

 
3) The melt sheet, comprising molten terrestrial rock, leaves the atmosphere and breaks into molten tektite ‘globules’. The globules form spheres, dumbbells or teardrops depending on the speed of rotation.

3) Lapisan yang meleleh, terdiri dari batuan yang mencair, meninggalkan atmosfer bumi dan pecah menjadi batu semi cair berbentuk bulatan-bulatan kecil (globules) yang bernama “tektite”. Globules ini membentuk bola, dumbbells atau air mata, tergantung pada kecepatan rotasi yang terjadi saat pembentukan batu tektites atau batu satam itu.

 

 
 

4) The Billitonite spheres, dumbbells and teardrops cool rapidly, so rapidly they form a glass (same, but not as pure, as in a modern wine or beer bottle).

4) Batu Satam yang berbentuk bola, dumbbells dan air mata mendingin dengan cepat, begitu cepat sehingga mereka membentuk kaca (sama dengan kaca, tetapi tidak murni, seperti di botol anggur atau bir modern).

 


5) Five/six or so minutes after impact the now solid sphere begins atmospheric re-entry over Belitung.

5) Sekitar lima hingga enam menit setelah tabrakan dengan asteroid terjadi, bola yang sekarang telah membeku dan menjadi solid mulai masuk kembali ke atmosfer bumi dan jatuh di Belitung.

 

6) As it re-enters at high velocity the friction of the tektite with the atmosphere heats up the anterior (front).

6) Karena Batu Satam itu memasuki kembali atmosfer bumi dengan kecepatan tinggi, gaya gesekan yang dialaminya memanaskan bagian depan dari batu ini.

 

 
7) When glass is unevenly heated (big difference between temperature at the front and back) it breaks. Think of pouring boiling water into a drinking glass.

7) Bila kaca dipanaskan dengan tidak merata (perbedaan temperatur yang besar antara bagian depan dan belakangnya), ia akan pecah. Seperti menuangkan air mendidih kedalam gelas minum.

  


8) Glass shards spall off the front of the Billitonite. Breakage is aided by intense deceleration pressures.

8) Bagian depan dari Batu Satam ini akan membentuk pecahan-pecahan kecil. Pecahan ini ditingkatkan juga oleh tekanan yang intens karena perlambatan kecepatan.


9) The Billitonite’s inherited cosmic velocity is eventually reduced and spalling ceases.

9) Kecepatan kosmik yang dibawa oleh momentum Batu Satam ini pada akhirnya akan berkurang dan pecahnya batuan juga akan berkurang.

   


10) The Billitonite falls to Earth by gravity in a more vertical path.

10) Karena ini Batu Satam akan jatuh ke bumi dengan gravitasi dengan gerakan yang lebih vertikal.

 


11) On the earth the Billitonite is transported by rivers and may be abraded.

11) Di bumi Batu Satam dibawa oleh air sungai dan mungkin tererosi.

  

 
12) Eventually the Billitonite is incorporated into sediment that also contains tin (eroded from hydrothermal deposits associated with the granite intrusion).

12) Pada akhirnya Batu Satam akan tergabung dengan endapan sediment yang biasanya juga mengandung timah (tererosi dari deposit panas bumi yang terkait dengan intrusi batu granit).


 

13) In the highly porous sands the acidic fresh waters of Belitung very slowly etch the Billitonite glass. Paper thin cracks (formed due to the glass being heated during atmospheric passage) are enlarged to U-grooves. Note that the U-grooves only form on the anterior (front) of the tektite, which was heated. The posterior surface retains it’s original spherical shape. Due to the acidic waters, tektites from Belitung are generally more heavily etched than tektites from other localities. This helps to give them a unique appearance and common 'mushroom-like' projections.

13) Di dalam tumpukan pasir yang berporositas tinggi, air tawar akan dengan sangat perlahan mengukir Batu Satam tersebut. Retakan setipis kertas (terbentuk karena gelas itu dipanaskan saat memasuki kembali atmosfer bumi) akan diperbesar dan membentuk parit kecil berbentuk U. Perhatikan bahwa parit berbentuk U ini hanya terbentuk di bagian yang terpanaskan, bagian depan dari Batu Satam (Tektite). Bagian belakang dari Batu Satam ini tetap seperti aslinya, berbentuk bola.

        

                   

                     

    


14) People mine for tin and discover Billitonites.

14) Orang-orang menambang timah dan menemukan Batu Satam.

 


15) People claim they are magical and mysterious. Magical/lucky stones are often associated with rarity.

15) Banyak orang yang menganggap Batu Satam ini berkhasiat (berkemampuan sihir) dan misterius. Batu berkhasiat dan beruntung sering dikaitkan dengan jarang didapat.


  


Discussion of Billitonites

‘Billitonite’ is a western name for tektites from Belitung Island in Indonesia (pronounced Bill-it-ung). The island was formerly known as Billiton Island and was part of the Dutch East Indies. In fact this is where the mining giant BHP Billiton derives part of its name. In 1860, the company, then just Billiton, acquired a concession to the tin-rich Billiton (now Belitung) island. This tin mining still goes on today and this is why tektites are found on this island. The tektites are locally referred to as Satam Stone, or sometimes Batu Satam. The word Satam comes from the language of the descendents of Chinese people who came to Belitung for work in the tin mines. SA means sand and TAM means gall: so Satam means bile sand (1).

On visiting the island, locals are keen to tell you that Satam Stone is only found in Belitung. This is what people believe, and you are not being lied to; however, this is only a partial truth. In Indonesia, tektites from the same impact can be found in several places in Kalimantan (Borneo), Natuna Islands, Gourd Island, Java Island aswell as Belitung Island (2). Barnes, 1963, reports Indonesian tektites from Kalimantan (Borneo) at Riam, Pleihari, Martapura and Laut; from Java Island at Sangiran and Japara and on the island of Flores at Mataloko. Outside of Indonesia tektites from the same impact are found in southernmost China Guangxi, Guangdong and Hainan provinces, Laos, Vietnam, Thailand, Cambodia, Myanmar, Philippines, Malaysia, Brunei, Australia and with microscopic tektites reaching as far as Antarctica.

The tektites in these different countries and localities have different forms and surface sculptures. This is principally a product of distance from the impact source –ground zero. The subsequent weathering, abrasion and chemical etching of the tektite, largely dependent on the rock and water chemistry in which the tektite is encased, will create further localised differences in tektite sculpture.

The Southeast Asian tektites were derived from an as yet undiscovered impact crater in Indochina, most likely located in the Bay of Tonkin. The Southeast Asian tektites can effectively be divided into 3 broad groups. Firstly the Indochinites which include tektites from Southern China, Vietnam, Laos, Cambodia and Thailand. These forms re-entered the atmosphere in a molten state, most molten in North Vietnam, Southern China and Northeast Thailand. Due to their molten re-entry they deformed into donut and onion shapes and suffered only limited thermal breakage of the anterior during re-entry.

The second subset, at intermediate distances from ground zero, includes Billitonites or Satam Stone, and Philippinites and Malaysianites. Basically tektites from Northern Indonesia, Malaysia and the Philippine Islands. These tektites re-entered the atmosphere as solid glass spheres. Frictional heating during atmospheric re-entry resulted in considerable spalling of the tektite body, leaving cores or ‘biscuits’.

The third subset, the most distal of the tektites, are the Australites. Similar forms also extend to the southernmost Indonesian areas (Java, Flores). These tektites, probably travelling at the greatest velocities and shallowest angles of re-entry and also entering as solid bodies, formed cores and the classic ablated button shape tektite.

Further afield, in Antarctica, only microtektites are found. Larger tektites would have been totally ablated away at this distance from the source crater.

So, Billitonites are tektites which formed at intermediate distances from the source crater and share common traits with tektites from Malaysia and the Philippines. In fact, if you muddle a lot of these tektites up you would struggle to tell the difference between a Billitonite and a Philippinite. Interestingly, whilst some are identical, a percentage of Billitonites are subtly different to the average Philippinites in that they have far more U-grooves than the average Philippinite.

Why do billitonites have more U-grooves than Philippinites? It may be that Billitonites formed marginally further from the source than Philippinites and are thus more cracked by frictional heating during re-entry. Billitonites were probably flung around 2,400 km from the source crater, Philippinites from Paracale some 1,700 km from the source crater and Philippintes from Davao some 2,400 km from the source crater. It is interesting to compare Desmond Leong’s ‘Shrek’ specimen from Davao with the Billitonites. Note that on this page the anterior with the projections is at the top. It would also be great to find a source for deeply etched specimens in Davao/Mindanao in the Philippines and compare these with Billitonites. The Philippinites currently coming from the Davao region are generally not deeply etched (less terrestrial alteration), which is equally pleasing.

An alternative suggestion as to why Billitonites have more U-grooves than Philippinites is that Billitonites may simply be less transported by terrestrial processes than the typical Philippinite, most of which come from Paracale, Bikol. If you ignore the chemically etched U-grooves then Billitonites, in general, appear less water worn. Phillipinites from Paracale, if water worn prior to etching, would have less cracks to attack and form U-grooves. In these Philippinites the abrasion may remove the top layer and so all small cracks are lost and only deeper cracks remain for chemical attack. More research needed on this front, but I think this scenario is less probable than it being a simple function of distance from the impact site. I would expect to see rare Philippinites from Bikol with many U-grooves like Billitonites if the sculpture was purely down to degree of water transportation prior to etching.

 

 

In Belitung the tektites are also, on average, smaller than those from Paracale, Philippines. I am told that no large breadcrust types are found. This is interesting. Belitung is some 700 km or so further from the impact site than Paracale, so on average one would expect smaller tektites and less breadcrusts. It appears, however, that breadcrust tektites formed from the same size spheres as ‘Biscuit’-forms. Perhaps the breadcrust forms were just perfect spheres and so initially (until a breakage/spalling occurred) had no fixed, stable flight orientation during early stages of re-entry. This being the case, given that we find 96g ‘biscuits’ in Belitung, pretty much the maximum size they can be, then very very rarely I would expect a breadcrust form in Belitung. These may not be found since the rarity of tektites in Belitung means a smaller sample set to work with.

After this trip I am very keen to obtain tektites in Mindanao, Philippines. This is where my wife is originally from and we will have many guests from Mindanao at our church wedding in February (we had a civil wedding earlier as I’m a foreigner). I will have to ask everyone to look for tektites!

 

References:

Reference (1) http://www.indosiar.com/news/sapa/74199/armageddon-di-pulau-belitung

Reference (2) http://www.jakartafair.biz/index.php?mid=288&lvl=2

Barnes V. E. 1963b. Tektite strewn fields. In: O'Keefe J. A (ed.) Tektites. Univiversity of Chicago Press, Chicago. 25-50.