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Suntikan Baru ICT Negara - Akademi Sains Malaysia

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fnside the earth<br />

lNslDE ths hot young<br />

Earth, haavy atoms such as<br />

iron were able to sink downwards<br />

lo the cetre, foming a<br />

liouid metalli coro of iron<br />

and nickel, possibly with a<br />

solid core at the cetre. Ths<br />

central tomoerature is<br />

around 4,00O'C.<br />

The lighter atoms, such<br />

as silicon, tloated upward<br />

around th6 outside of lhe<br />

core and formed the mantle.<br />

Above this floats an ever<br />

changing thin crust 10 to 30<br />

km thick.<br />

The Earth's inner core is a solid 2432 km across, probably<br />

lormed mostly from heavy atoms such as iron and uranium.<br />

Around this is a liouid outer core 2270 km thick made of iron and<br />

lighter aloms such as orygen and sulfur.<br />

Around lhe core is lhg mantle.<br />

The Earth's magnetic field is lhoughto originate in the core.<br />

The core is believed to be kepl warm by radioactive decay.<br />

Rocky Snowballs<br />

As the Earth formed out of<br />

roclq snowballs it glow hot and<br />

probably melted. One theory is<br />

that early in its history a large<br />

obtecr hit the Earth, which threw<br />

out a shower of rocks. These<br />

collected logether to torm lhe<br />

Moon. ll il is true this would certainly<br />

havs made the Earlh melt.<br />

The grazing impact ol a Marssized<br />

body with the proto-earth<br />

more than lour billion years ago<br />

is believed to have lsd to the tormation<br />

of our moon.<br />

About 300 thousand ygars atl€r<br />

ths Big Bang, the Universe had<br />

cooled lo be captured by protons<br />

and alpha particlss lo iorm atoms.<br />

An elsctron is pull€d towards a<br />

proton because their oppositg 9l6ctric<br />

cfiarges attract each olher.<br />

They stick tog€thsr to form a totally<br />

n€w kind of object callod an atom<br />

ol hydrogen. In the same way two<br />

slectrons were altracrtad to each alpha particle, whlch contained<br />

two protons, and wer€ hsld doss to it. The alom lhey mad€ is<br />

called a h€lium atom.<br />

Atoms are tantastic things. Around the oulsids ol the atom the<br />

€lectron forms a lafgo, thin sh6ll. Insid€ ths alom is smpty space,<br />

except for the tiny heavy proton at ths csntre. An atom is like a<br />

lootball.<br />

The electron in an atoms is like tha skin of lh€ foolball. Undor<br />

this skin the atom is almost smpty. At lhs c€ntre is somothing a<br />

football doesn't have. Hsld at the center by lho olectric lorc€ is<br />

the tiny proton. This is called the nusleus of the atom- Ths young<br />

Universe was tull of hol atoms, moving around and bouncing off<br />

each olhs( They made a gas.<br />

Onc€ all lhe el€ctrons were atoms trapped in aloms, the fog ot<br />

the Universo cieared.<br />

zzesti}otmq<br />

o<br />

The Crust<br />

The crust of th6 Earth is a thin dgid layer<br />

of rock. lt ffoats on lhg mantle.<br />

It is made mostly of a layer of dark rock<br />

called basalt and is 5-10 km thick. The<br />

oceans lie above this layer. Trapped in this<br />

basalt are lumps ol thicksr rocks similar to<br />

granite, 30 - 40 km thick. These lumps stick<br />

orjt of the oceans to form lhe @ntinents.<br />

Oceanlc crust

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