Report On the Bore of the Tsien-Tang Kiang
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VIII. 30 8 11 H.
5 L.
13 11 H.
IX.
10 4 H.
4 8 L.
15 H.
IX. 30 11 1 H.
4 6 L.
15 7 H.
X.
10 2 H.
3 8 L.
13 10 H.
X. 30 5 1 H.
2 10 L.
7 11 H.
XI.
3 H.
1 7 L.
1 10 H.
XL 30 1 5 L.
6 H.
11 L.
Noon.
3 L.
5 H.
4 1 L.
0. 30 4 6 L.
1 7 H.
6 1 L.
I.
5 4 L.
2 5 H.
7 9 L.
1.30 6 2 L.
3 2 H.
9 4 L.
11.
7 4 L.
3 4 H.
10 8 L.
11.30 8 2 L.
3 7 H.
11 9 L.
III.
8 7 L.
3 10 H.
12 5 L.
This table shows that two hours before high water at Changtau, when the apex of the tidal wave is over the deep water of the oc...ean, there is a difference of level of 15 feet between the water at Changtau harbour and Rambler island. There is no indication of remarkable pressure at West Volcano island, which is at the mouth of the Hang-chau gulf; but an hour later, when the apex of the wave is nearing the Chusan archipelago, there is great pressure on the water in the Hang-chau estuary and the difference of level of the water between Changtau and Rambler island reduces 13. feet in one hour and a half. Judging by the analagous case of Changtau and West Volcano, the strongest flood stream would be when this difference is reduced by one half, that is to say, when the water is in its full swing of effort to regain equilibrium.
What to read after Report On the Bore of the Tsien-Tang Kiang?
You can find similar books in the "Read Also" column, or choose other free books by William Usborne Moore to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
VIII. 30 8 11 H.
5 L.
13 11 H.
IX.
10 4 H.
4 8 L.
15 H.
IX. 30 11 1 H.
4 6 L.
15 7 H.
X.
10 2 H.
3 8 L.
13 10 H.
X. 30 5 1 H.
2 10 L.
7 11 H.
XI.
3 H.
1 7 L.
1 10 H.
XL 30 1 5 L.
6 H.
11 L.
Noon.
3 L.
5 H.
4 1 L.
0. 30 4 6 L.
1 7 H.
6 1 L.
I.
5 4 L.
2 5 H.
7 9 L.
1.30 6 2 L.
3 2 H.
9 4 L.
11.
7 4 L.
3 4 H.
10 8 L.
11.30 8 2 L.
3 7 H.
11 9 L.
III.
8 7 L.
3 10 H.
12 5 L.
This table shows that two hours before high water at Changtau, when the apex of the tidal wave is over the deep water of the oc...ean, there is a difference of level of 15 feet between the water at Changtau harbour and Rambler island. There is no indication of remarkable pressure at West Volcano island, which is at the mouth of the Hang-chau gulf; but an hour later, when the apex of the wave is nearing the Chusan archipelago, there is great pressure on the water in the Hang-chau estuary and the difference of level of the water between Changtau and Rambler island reduces 13. feet in one hour and a half. Judging by the analagous case of Changtau and West Volcano, the strongest flood stream would be when this difference is reduced by one half, that is to say, when the water is in its full swing of effort to regain equilibrium.
What to read after Report On the Bore of the Tsien-Tang Kiang?
You can find similar books in the "Read Also" column, or choose other free books by William Usborne Moore to read onlineMoreLess
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