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!Solar/Describe/Earth

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Filename: !Solar/Describe/Earth
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File contents
Earth is the third planet from the Sun. It is the first planet 
from the Sun to have a moon, a common feature for all the 
other planets beyond our orbit. The Earths atmosphere reaches 
to approximately 80km above the surface, but this is only 
about one-hundredth of the planets radius, and so occupies a
relatively thin band around the planet.  It is composed mainly 
of Nitrogen (78%) and oxygen (21%) with the remainder built up 
from small traces of other gases. These relative proportions 
remain fairly constant up to around 80km, but the heavy gases 
become rare at greater heights and only hydrogen and helium 
are found in the outermost regions. At the height of the 
stratosphere there is a concentrated layer of ozone, at about 
25km. This ozone layer is vital to life on the planet, as it 
stops nearly all of the Suns harmful ultraviolet radiation 
from reaching the surface.

The Earths atmosphere also contains a large amount of water 
vapour, although its concentration varies in different places 
and is subject seasonal variations. Most of it is visible as 
clouds, and most of these extend only to the top of the 
troposphere, up to 13km. It is in this region that the 
dominant weather systems are found. Above this lies a layer of 
warm air which holds cooler air below containing most of the 
water vapour, and the clouds that we see.

The surface of the planet is subject to much Geological 
activity, and is shaped by continental drifting (Plate 
tectonics). This makes the planets surface relatively young, 
and taken in account with other factors such as the existence 
of an atmosphere and  weathering, explains why few visible 
impact craters are to be found, unlike for example on the 
surface of the moon, which is heavily cratered, and gives a 
more accurate guide as to the quantity of collisions with 
debris making its way through the solar system. Here the 
surface features date back to the formation of the solar 
system, and have remained undisturbed due to the moons 
geological inactivity.

The structure of the planet itself is divided into three 
regions, the crust which extends for roughly 7km beneath the 
oceans and 40km beneath the continents, the mantle which is 
roughly 2870km thick, and the core which accounts for the 
remaining 3480km. This core is composed of two layers, the 
inner is solid, the outer flows. They are both composed mainly 
of iron, and it is convection in the molten outer layer that 
plays an important role in accounting for the planets magnetic 
field.

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00000020  68 65 20 53 75 6e 2e 20  49 74 20 69 73 20 74 68  |he Sun. It is th|
00000030  65 20 66 69 72 73 74 20  70 6c 61 6e 65 74 20 0a  |e first planet .|
00000040  66 72 6f 6d 20 74 68 65  20 53 75 6e 20 74 6f 20  |from the Sun to |
00000050  68 61 76 65 20 61 20 6d  6f 6f 6e 2c 20 61 20 63  |have a moon, a c|
00000060  6f 6d 6d 6f 6e 20 66 65  61 74 75 72 65 20 66 6f  |ommon feature fo|
00000070  72 20 61 6c 6c 20 74 68  65 20 0a 6f 74 68 65 72  |r all the .other|
00000080  20 70 6c 61 6e 65 74 73  20 62 65 79 6f 6e 64 20  | planets beyond |
00000090  6f 75 72 20 6f 72 62 69  74 2e 20 54 68 65 20 45  |our orbit. The E|
000000a0  61 72 74 68 73 20 61 74  6d 6f 73 70 68 65 72 65  |arths atmosphere|
000000b0  20 72 65 61 63 68 65 73  20 0a 74 6f 20 61 70 70  | reaches .to app|
000000c0  72 6f 78 69 6d 61 74 65  6c 79 20 38 30 6b 6d 20  |roximately 80km |
000000d0  61 62 6f 76 65 20 74 68  65 20 73 75 72 66 61 63  |above the surfac|
000000e0  65 2c 20 62 75 74 20 74  68 69 73 20 69 73 20 6f  |e, but this is o|
000000f0  6e 6c 79 20 0a 61 62 6f  75 74 20 6f 6e 65 2d 68  |nly .about one-h|
00000100  75 6e 64 72 65 64 74 68  20 6f 66 20 74 68 65 20  |undredth of the |
00000110  70 6c 61 6e 65 74 73 20  72 61 64 69 75 73 2c 20  |planets radius, |
00000120  61 6e 64 20 73 6f 20 6f  63 63 75 70 69 65 73 20  |and so occupies |
00000130  61 0a 72 65 6c 61 74 69  76 65 6c 79 20 74 68 69  |a.relatively thi|
00000140  6e 20 62 61 6e 64 20 61  72 6f 75 6e 64 20 74 68  |n band around th|
00000150  65 20 70 6c 61 6e 65 74  2e 20 20 49 74 20 69 73  |e planet.  It is|
00000160  20 63 6f 6d 70 6f 73 65  64 20 6d 61 69 6e 6c 79  | composed mainly|
00000170  20 0a 6f 66 20 4e 69 74  72 6f 67 65 6e 20 28 37  | .of Nitrogen (7|
00000180  38 25 29 20 61 6e 64 20  6f 78 79 67 65 6e 20 28  |8%) and oxygen (|
00000190  32 31 25 29 20 77 69 74  68 20 74 68 65 20 72 65  |21%) with the re|
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000001d0  65 73 2e 20 54 68 65 73  65 20 72 65 6c 61 74 69  |es. These relati|
000001e0  76 65 20 70 72 6f 70 6f  72 74 69 6f 6e 73 20 0a  |ve proportions .|
000001f0  72 65 6d 61 69 6e 20 66  61 69 72 6c 79 20 63 6f  |remain fairly co|
00000200  6e 73 74 61 6e 74 20 75  70 20 74 6f 20 61 72 6f  |nstant up to aro|
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00000220  65 20 68 65 61 76 79 20  67 61 73 65 73 20 0a 62  |e heavy gases .b|
00000230  65 63 6f 6d 65 20 72 61  72 65 20 61 74 20 67 72  |ecome rare at gr|
00000240  65 61 74 65 72 20 68 65  69 67 68 74 73 20 61 6e  |eater heights an|
00000250  64 20 6f 6e 6c 79 20 68  79 64 72 6f 67 65 6e 20  |d only hydrogen |
00000260  61 6e 64 20 68 65 6c 69  75 6d 20 0a 61 72 65 20  |and helium .are |
00000270  66 6f 75 6e 64 20 69 6e  20 74 68 65 20 6f 75 74  |found in the out|
00000280  65 72 6d 6f 73 74 20 72  65 67 69 6f 6e 73 2e 20  |ermost regions. |
00000290  41 74 20 74 68 65 20 68  65 69 67 68 74 20 6f 66  |At the height of|
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000002d0  20 6f 66 20 6f 7a 6f 6e  65 2c 20 61 74 20 61 62  | of ozone, at ab|
000002e0  6f 75 74 20 0a 32 35 6b  6d 2e 20 54 68 69 73 20  |out .25km. This |
000002f0  6f 7a 6f 6e 65 20 6c 61  79 65 72 20 69 73 20 76  |ozone layer is v|
00000300  69 74 61 6c 20 74 6f 20  6c 69 66 65 20 6f 6e 20  |ital to life on |
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00000320  74 20 0a 73 74 6f 70 73  20 6e 65 61 72 6c 79 20  |t .stops nearly |
00000330  61 6c 6c 20 6f 66 20 74  68 65 20 53 75 6e 73 20  |all of the Suns |
00000340  68 61 72 6d 66 75 6c 20  75 6c 74 72 61 76 69 6f  |harmful ultravio|
00000350  6c 65 74 20 72 61 64 69  61 74 69 6f 6e 20 0a 66  |let radiation .f|
00000360  72 6f 6d 20 72 65 61 63  68 69 6e 67 20 74 68 65  |rom reaching the|
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00000380  61 72 74 68 73 20 61 74  6d 6f 73 70 68 65 72 65  |arths atmosphere|
00000390  20 61 6c 73 6f 20 63 6f  6e 74 61 69 6e 73 20 61  | also contains a|
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000003c0  61 6c 74 68 6f 75 67 68  20 69 74 73 20 63 6f 6e  |although its con|
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00000400  62 6a 65 63 74 20 73 65  61 73 6f 6e 61 6c 20 76  |bject seasonal v|
00000410  61 72 69 61 74 69 6f 6e  73 2e 20 4d 6f 73 74 20  |ariations. Most |
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00000430  20 61 73 20 0a 63 6c 6f  75 64 73 2c 20 61 6e 64  | as .clouds, and|
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000004e0  72 20 6f 66 20 0a 77 61  72 6d 20 61 69 72 20 77  |r of .warm air w|
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00000560  65 20 70 6c 61 6e 65 74  20 69 73 20 73 75 62 6a  |e planet is subj|
00000570  65 63 74 20 74 6f 20 6d  75 63 68 20 47 65 6f 6c  |ect to much Geol|
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00000590  2c 20 61 6e 64 20 69 73  20 73 68 61 70 65 64 20  |, and is shaped |
000005a0  62 79 20 63 6f 6e 74 69  6e 65 6e 74 61 6c 20 64  |by continental d|
000005b0  72 69 66 74 69 6e 67 20  28 50 6c 61 74 65 20 0a  |rifting (Plate .|
000005c0  74 65 63 74 6f 6e 69 63  73 29 2e 20 54 68 69 73  |tectonics). This|
000005d0  20 6d 61 6b 65 73 20 74  68 65 20 70 6c 61 6e 65  | makes the plane|
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000005f0  69 76 65 6c 79 20 79 6f  75 6e 67 2c 20 0a 61 6e  |ively young, .an|
00000600  64 20 74 61 6b 65 6e 20  69 6e 20 61 63 63 6f 75  |d taken in accou|
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00000620  63 74 6f 72 73 20 73 75  63 68 20 61 73 20 74 68  |ctors such as th|
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00000640  61 6e 20 61 74 6d 6f 73  70 68 65 72 65 20 61 6e  |an atmosphere an|
00000650  64 20 20 77 65 61 74 68  65 72 69 6e 67 2c 20 65  |d  weathering, e|
00000660  78 70 6c 61 69 6e 73 20  77 68 79 20 66 65 77 20  |xplains why few |
00000670  76 69 73 69 62 6c 65 20  0a 69 6d 70 61 63 74 20  |visible .impact |
00000680  63 72 61 74 65 72 73 20  61 72 65 20 74 6f 20 62  |craters are to b|
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000007e0  61 6c 20 69 6e 61 63 74  69 76 69 74 79 2e 0a 0a  |al inactivity...|
000007f0  54 68 65 20 73 74 72 75  63 74 75 72 65 20 6f 66  |The structure of|
00000800  20 74 68 65 20 70 6c 61  6e 65 74 20 69 74 73 65  | the planet itse|
00000810  6c 66 20 69 73 20 64 69  76 69 64 65 64 20 69 6e  |lf is divided in|
00000820  74 6f 20 74 68 72 65 65  20 0a 72 65 67 69 6f 6e  |to three .region|
00000830  73 2c 20 74 68 65 20 63  72 75 73 74 20 77 68 69  |s, the crust whi|
00000840  63 68 20 65 78 74 65 6e  64 73 20 66 6f 72 20 72  |ch extends for r|
00000850  6f 75 67 68 6c 79 20 37  6b 6d 20 62 65 6e 65 61  |oughly 7km benea|
00000860  74 68 20 74 68 65 20 0a  6f 63 65 61 6e 73 20 61  |th the .oceans a|
00000870  6e 64 20 34 30 6b 6d 20  62 65 6e 65 61 74 68 20  |nd 40km beneath |
00000880  74 68 65 20 63 6f 6e 74  69 6e 65 6e 74 73 2c 20  |the continents, |
00000890  74 68 65 20 6d 61 6e 74  6c 65 20 77 68 69 63 68  |the mantle which|
000008a0  20 69 73 20 0a 72 6f 75  67 68 6c 79 20 32 38 37  | is .roughly 287|
000008b0  30 6b 6d 20 74 68 69 63  6b 2c 20 61 6e 64 20 74  |0km thick, and t|
000008c0  68 65 20 63 6f 72 65 20  77 68 69 63 68 20 61 63  |he core which ac|
000008d0  63 6f 75 6e 74 73 20 66  6f 72 20 74 68 65 20 0a  |counts for the .|
000008e0  72 65 6d 61 69 6e 69 6e  67 20 33 34 38 30 6b 6d  |remaining 3480km|
000008f0  2e 20 54 68 69 73 20 63  6f 72 65 20 69 73 20 63  |. This core is c|
00000900  6f 6d 70 6f 73 65 64 20  6f 66 20 74 77 6f 20 6c  |omposed of two l|
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00000920  72 20 69 73 20 73 6f 6c  69 64 2c 20 74 68 65 20  |r is solid, the |
00000930  6f 75 74 65 72 20 66 6c  6f 77 73 2e 20 54 68 65  |outer flows. The|
00000940  79 20 61 72 65 20 62 6f  74 68 20 63 6f 6d 70 6f  |y are both compo|
00000950  73 65 64 20 6d 61 69 6e  6c 79 20 0a 6f 66 20 69  |sed mainly .of i|
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00000970  6f 6e 76 65 63 74 69 6f  6e 20 69 6e 20 74 68 65  |onvection in the|
00000980  20 6d 6f 6c 74 65 6e 20  6f 75 74 65 72 20 6c 61  | molten outer la|
00000990  79 65 72 20 74 68 61 74  20 0a 70 6c 61 79 73 20  |yer that .plays |
000009a0  61 6e 20 69 6d 70 6f 72  74 61 6e 74 20 72 6f 6c  |an important rol|
000009b0  65 20 69 6e 20 61 63 63  6f 75 6e 74 69 6e 67 20  |e in accounting |
000009c0  66 6f 72 20 74 68 65 20  70 6c 61 6e 65 74 73 20  |for the planets |
000009d0  6d 61 67 6e 65 74 69 63  20 0a 66 69 65 6c 64 2e  |magnetic .field.|
000009e0  0a 0a                                             |..|
000009e2