Hyphenated word was joined on the previous page because of the intervening image, and the second footnote was moved to the next page where it's supposed to belong. — Ineuw talk 11:50, 10 December 2013 (UTC) (Wikisource contributor note)
| Fig. 4. Low Isolated Mountain Group in Northeastern China. Fig. 5. Two Farmers Raising Water from the Grand Canal into the Head of an Irrigating Ditch by means of a Wicker Basket slung between them. |
Fig. 6. A wide River Plain among the Mountains of Shan-tung. The bridge of stone slabs across the sand laden river is part of the principal wheel-barrow road of the valley. Fig. 7. A Typical City Wall, with Gate Tower. |
largely by the rocks of which it consists, partly by the climate to which it has been subject, but chiefly by the geologic events which have occurred during its history. Of course the beginnings of that history are unknown, just as the human history of China shades into darkness when we attempt to trace it back into the remote ages. But the present features of the land are chiefly due to the later events in its life, and these have been partly worked out by the geologists who have explored its surface.
We may take as a convenient starting point for our interpretation a time far back in geologic chronology[1] when China was a land surface which had been exposed to erosion so long that nearly all the hills and mountains that may have existed there before had been worn away, leaving a relatively flat plain with groups of low hills here and there. The rocks beneath this plain were of various kinds, most of them highly folded. Eventually this surface was submerged beneath a comparatively shallow inland sea, and although the uneasy movements of the earth's body caused the sea bottom to emerge occasionally, it remained below the water nearly all through the geologic periods which constitute the Paleozoic era. By the end of that time we may picture China as a shallow sea bottom rising very gradually to a marshy coastal plain on the east. During the long intervening ages the accumulation of sediments upon the sea bottom had formed successive layers of limestone,
- ↑ Just before the Cambrian period.
