စိတ္ရြက္လြင္႔ရာ-ရကိၡတ စာမ်က္ႏွာ(TAT၈၆Bumi)

Friday, May 27, 2016

ဘူမိ သီခ်င္းမ်ား

Geology Songs

ဘူမိညီအကိုမ်ား အတြက္ ကမၻာအရပ္ရပ္က
ဘူမိခ်စ္သူမ်ားရဲ့ ဘူမိသီခ်င္းေတြကိုစုစည္းတင္ေပးလိုက္ပါတယ္၊
ကိုယ္ပိုင္သံစဥ္၊ ေကာ္ပီသံစဥ္ေတြလဲပါသလို
  ျမန္မာ ဘူမိသီခ်င္းႏွစ္ပုဒ္သာမဟုတ္
 Department of Earth Science at Cambridge University  ရဲ႕ 
 ေက်ာင္းသားကေန အေမရိကန္ Tennessee သားရဲ႕ ေရးဖြဲ႕ သီဆိုမႈ ႐ုရွား တို႕ရဲ႕ ဘူမိသီခ်င္း ထိ  ပါေပမယ့္
သူတို႕ ေရးဖြဲ႕တာ ဘူမိပညာရပ္ရဲ႕ အေၾကာင္းအရာေတြကို စပ္ဆိုထားတာကမ်ားၿပီး
ဘူမိညီအစ္ကို ကိုေက်ာ္ေက်ာ္မင္း ေရးဖြဲ႕စပ္ဆိုခဲ့တဲ့ ဘူမိေက်ာင္းေတာ္သား ဆိုတဲ့
 ျမန္မာဘူမိေက်ာင္းသားေတြရဲ႕ အေတြ႕အႀကံု ခံစားခ်က္ကို အသားေပးေရးသားတဲ့ သီခ်င္းကို မမီွဘူးလို႕ဆိုခ်င္ပါတယ္
 အားလံုးတူညီတဲ့ တစ္ခ်က္က ခပ္ေျပာင္ေျပာင္ေတြ ဆိုတာပါဘဲ။
Short Film ေလးတစ္ခုလည္း line ေပၚေတြ႕တာနဲ႕ ေအာက္ဆံုးမွာ ထည္႔႐ွယ္လိုက္ပါတယ္။

Tat86Bumi 
 
က်ေနာ္ကေတာ့ ဒီသီခ်င္းကို Geology of Tennessee လို႕အမည္ေပးခ်င္ပါရဲ႕


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Geology Pie with super trooper intrusion လို႕ နံမည္ေပးရမည္လားမသိ American pie ဆိုတဲ့သံစဥ္ မွာ ABBA ရဲ႕ Super trooper သီခ်င္းသံစဥ္ကို intrusion လုပ္ထဲ့ထားၿပီး စာသားေကာ္ပီသြင္းထားတာမို႕ ဘူမိသီခ်င္းပိုဆန္သြားတယ္ေျပာရမည္လားမသိပါ။
 Published on May 2, 2014
Written by Matthew Kemp and Lizzie Pearmain (2014)
With Christopher Matthews and Arran Group B
Dedicated to the Demonstrators of Arran Group B
 Filmed by Tom Perkins during the 1A recruitment lunch on Wednesday 30.04.2014 in the Department of Earth Sciences Watson Gallery (aka the common room) at the University of Cambridge.
This is a song about the Geology of Arran, which is geologically accurate (mostly...) and could hopefully help with revision! Imagine it being sung to the tune of 'American Pie' by Don McLean (though it was influenced by the 'The Saga Begins' version by Weird Al Yankovic) and the 'Abba Intrusion' to the tune of 'Super Trouper'. Also, a lot of the rhymes are tenuous at best, so use your imagination to make it work! Geologise!!!

Lyrics:
Geology of Arran Song

A long, long time ago,
About 400 million years or so,
Back in the Ordovician,
The Iapetus Ocean began to close,
Continents collided and the seafloors rose,
Right up to the start of the Silurian.

We saw some rocks from the Bouma series,
Which was consistent with our theories,
That these formed on the continental slope,
Down which dense sediment did elope.
And when England collided with an island arc,
Volcanic eruptions occurred, with mafic minerals dark,
Their bulbous glassy margins have made their mark,
On the Ayrshire coast.

So my, my this here ophiolite,
Brought the sea floor to the surface and out into the light,
Check those pillow lavas and those coarse turbidites,
The geology on the coast is alright,
The geology on the coast is alright.

But then we went to Arran; there were so many rocks,
From all the different eras and most of the epochs,
And a few unconformities were seen.
There were cross-bedded, red, well-sorted sands
From the hot, arid deserts of the Permian;
Water table rises were inferred by honeycomb weathering.

We saw cyclothems from the Carboniferous.
It looked like these rocks had been put here for us.
There were deltas; lime and siltstones,
And even some fossils of bryozoans.
Then we saw something quite bizarre;
A coarse conglomerate or a breccia;
Flash floods had created a massive lahar,
Right next to the Devonian Old Red.

So my, my this geology guys.
We thought Arran was so barren, but now that's just a lie.
Put our hard hats on and kissed our clean boots goodbye,
Singing geology's like traveling in time,
Geology's like traveling in time.

BAKED MARGIN
Abba Intrusion!!!
Dalradian Super Group-per,
It's a meta-sediment,
Looks like it's a schist,
Why do we care about this?
Because we're all geologists.
BAKED MARGIN

These rocks dated back to the Pre-Cambrian,
And whoa -- the schist has hit the alluvial fan;
The turbidite sequence got metamorphosed.
We mapped out the valley of North Glen Sannox,
By identifying rock types at lots of outcrops,
To check the lithology that had been proposed.

If there's Triassic beds with footprints of dinos,
Then work out the dip with your compass-clinos.
It's all intruded by dykes,
And if you work out their strikes,
They lead to a sill made from Quartz-Feldspar Porphyry,
Which all upwelled during the Tertiary;
The pluton in the middle looks quite like G5A,
All caused by a hot spot.

Chorus

There were some rocks from the Jurassic and Cretaceous,
But they were quite boring, and not that siliceous,
And some glacial erratics from the Quaternary.
The conjugated kink bands and folded beds
Made it much clearer in our heads
About the wide-scale orogeny.

And by the sill of Drumadoon,
We swear that we will come back soon,
When our knowledge of rocks is greater,
Like that of our amazing demonstrators.
Our highlights include Hutton's Unconformity,
And also the meal enhanced by BP.
From this week it's plain to see:
We all love Geology!

Chorus × 2
Geologise!!!
  • Category

  • License

    • Standard YouTube License

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