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Sun 94 Posted 16 years ago
Essay & Composition Writing

A volcanic islands

I am trying to summarize the underlined parts and if you see any mistakes, can I have your comments?

At the place where the formation of such an island begins, the sea floor is probably nowhere more than about fifty miles thick. In it are deep cracks and fissures, the results of unequal cooling and shrinkage in past ages. Along such lines of weakness the molten lava from the earth's interior presses up and finally bursts forth into the sea

__> along the wekaend lines of the sea floor, the forces of the earth pushed up the lava and it flies up the sea.
  

Top answer

Hi, I am trying to summarize the underlined parts and if you see any mistakes, can I have your comments? At the place where the formation of such an island begins, the sea floor is probably nowhere more than about fifty miles thick. In it are deep cracks and fissures, the results of unequal cooling and shrinkage in past ages.

  • Hi, I am trying to summarize the underlined parts and if you see any mistakes, can I have your comments?
  • At the place where the formation of such an island begins, the sea floor is probably nowhere more than about fifty miles thick.
  • In it are deep cracks and fissures, the results of unequal cooling and shrinkage in past ages.
  • Along such lines of weakness the molten lava from the earth's interior presses up and finally bursts forth into the sea __> along the wekaend lines of the sea floor, the forces of the earth pushed up the lava and it flies up the sea.
  • __> Along these weakened lines on the sea floor, the lava pushes up until it flies up into the sea.
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1 Answers
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Hi,

I am trying to summarize the underlined parts and if you see any mistakes, can I have your comments?

At the place where the formation of such an island begins, the sea floor is probably nowhere more than about fifty miles thick. In it are deep cracks and fissures, the results of unequal cooling and shrinkage in past ages. Along such lines of weakness the molten lava f

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