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THREAD

"How does Earth 'Manufacture' Land?
Some aspects of Natural History in the Indian Context"

The witticism “Buy Land. They ain't making any more of the stuff” is true, of course, if we look at “normal” time scales.

But it is not true on geological time scales!
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This Thread is an attempt to answer a question which came to me when writing a previous Thread (Roopkund Skeletons – see my Pinned Tweet).

Did Earth have land and mountains and rivers and valleys on it ever since its birth 4.53 billion years ago?
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The following is an attempt to explain what I was able to discover on the topic.

(Like my other Threads this one is also basically Notes which I made to understand the topic. I am not an expert. Do point out any mistakes when you find them).
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Here goes.

The Universe started with the Big Bang 13.8 billion years ago.

The consequent expansion of Energy and Space led to formation of particles.

Later these particles started clumping together to form simple atoms – Hydrogen and Helium.

(image from Wikipedia)
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For half a billion years the Universe was dark.

But clumps of H and He were growing in size. They grew so massive that atoms in their interior, crushed by the pressure of the outer material, started fusing into heavier atoms.
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Fusion releases energy.

These were the first stars. There was Light!

As fusion proceeded, even heavier atoms, like iron, formed.

But star fuel ultimately runs out. If the star is large, it explodes – a “nova” or “supernova”.
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These explosions spew out matter into space forming dust and gas clouds called nebulae.

At some point nearby particles in a nebula start sticking together due to static electricity. They attract more particles.

("Pillars of Creation" in Eagle Nebula-from Wikipedia)
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With more mass, gravity takes over. The nebula starts collapsing. A new star forms.

Left over dust and gas settle down as a “protoplanetary” disk revolving around the star. The material in this protoplanetary disk may gradually coalesce into planets.
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Our solar system also formed this way.

Inner planets - Mercury to Mars - were so hot that only iron and silicates could crystallise. These planets are rocky.

Jupiter, Saturn became gas giants.

Neptune, Uranus are ice giants where all gases crystallised.
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At its birth 4.53 billion years ago Earth was very hot.

This was partly due to energy present in the proto planetary disk.

Other reasons were radioactive decay, collisions with other objects (one of which formed the moon) and compression due to gravity.
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For the first half billion years after its birth Earth actually kept getting hotter because of these reasons.

A critical point came when its temperature exceeded the melting point of Iron (about 1500 deg C). This is called the “Iron Catastrophe”.
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Molten Iron, Nickel and other dense elements started trickling downwards through the lighter molten silicates and other minerals.

Friction from the trickling down of molten metal added to the heat.
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So the material on Earth got rearranged.

Heavier elements, like iron and nickel, wound up at Earth's centre – forming its Core. The lighter silicates surrounded the Core, forming the next layer - the “Mantle”.
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Today Earth's Core is a 3500 km thick ball of Iron and Nickel.

At its centre, about 6400 km down, temperature is ~6000 deg C.

But despite the high temperature Iron and Nickel in the Core are in solid form because of the pressure of the material above!
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Above the Core, starting about 2900 km down and extending up almost to earth's surface, is the Mantle. The temperature at its base is about 3500 deg C.

It is composed of molten silicates with very high Magnesium and Iron content - “Ultra Mafic” rock.
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The upper layer of the Mantle, the Aesthenosphere, is cooler, and consists mostly of solid rock.

But convection from inner layers means that molten rock also comes through. Asthenosphere is therefore fluid, and not very strong.
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Above the Mantle is the “Crust”. It consists of solid rock, about 15 km thick on average, but much thicker in places. Temperature at its base is about 1000 deg C. The Crust floats on the Aesthenosphere below.
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The outermost Mantle and the Asthenosphere below it are together called the Lithosphere.

The Crust is not a single piece, but multiple pieces. These pieces are called “tectonic plates”.
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Pieces of the Crust with more silicates (“Felsic”), are lighter and “ride higher” while floating. They form the Crust under land.

Other pieces, with more Magnesium and Iron (“Mafic”), are denser and “sink” lower. They form the Crust below oceans.
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In 1911 Alfred Wegener observed that many different continents have similar fossils.

He proposed that since these organisms could not have crossed oceans, the landmasses where they are found must have been joined at one time, and then moved apart.
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The idea did not find acceptance at first. But over time more evidence for Wegener's hypothesis emerged.

One of these was related to earth's magnetism.
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Free Haematite (Fe3O4 - Iron Oxide) particles on earth's surface, being magnetic, point north.

But haematite embedded in rocks of different ages in different continents over last few hundred million years, points in various different directions.
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Since north pole has stayed stationary over this time, the only explanation is that haematite was indeed pointing north when it got embedded in rock, but that subsequently the landmass itself moved and changed direction.
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By studying the orientation of haematite particles it is actually possible to deduce what latitude the underlying landmass was at, when the particle got embedded in rock.

This evidence led to the theory of “Plate Tectonics” being accepted by the 1960s.
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The accepted wisdom now is that about 150 - 200 m years ago there was a super continent - Pangaea.

Then the Plates started moving and Pangaea started to break up.

After 200 million years of drift the Plates reached their present positions.
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200 m years ago, Africa split from Asia, N America from S America, Atlantic began to open up between N Africa and N America and India split from Antarctica. S America later split from Africa and N America from Europe. India moved north.
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Africa separated from S America and Europe from N America 80 m years ago.

Australia separated from Antarctica and India collided with Asia 50 m years ago.

(For context, note that 200 m yrs is a mere blip compared to 4.53 b yrs, the age of the earth).
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This drifting of Plates will continue into the future.

Perhaps 250 million years from now, the continents will be together again.

Many similar cycles of separation and merger (called Wilson Cycles – after J Tuzo Wilson) were there before Pangaea.
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But why did a super continent like Pangaea break up?

Wilson proposed that breakup started at points where hot Magma from Earth's Mantle rises to the Crust in a “Plume”. This weakens the Crust and leads to formation of separate Tectonic Plates.
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Different Tectonic Plates move in different directions.

At places different Plates diverge from each other. At other places they collide with each other. At yet other places they slide past each other.
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