56 
PROGRESS REPORT, HYDROGRAPHY, 1893 AND 1894. [bull.iih. 
and 20 feet north of the cable. The elevation is 2.35 feet above the 
5-foot mark of the gage. The gage was found to be apparently 
solid, but it was evident that the ice around the lower portion had 
lifted that end, necessitating a correction in the original markings. 
The changes at this point due to ice in the river necessitate the con- 
struction of a different form of gage in order to give comparable 
readings. The following table gives the heights of river as reported 
by the observer : 
Daily gage height of Bear River at Collinston, Utah, for 1893. 
Day. 
Jan. 
Feb. 
Mar. 
Apr. 
May. 
June. 
July. 
Aug. 
Sept. 
Oct. 
Nov. 
Dec. 
1 
2.10 
2.10 
1.90 
3.50 
4.10 
4.90 
4.05 
1.90 
1.60 
1.90 
2.10 
2.40 
2 
2.05 
2.15 
1.90 
3.55 
4.10 
4.85 
4.00 
1.90 
1.60 
1.90 
2.10 
2.40 
3 
2.00 
2.10 
1.80 
3.80 
4.20 
4.80 
3.90 
2.00 
1.60 
1.90 
2.20 
2.40 
4 
2.10 
2.00 
1.80 
3.90 
4.20 
4.90 
3.80 
2.00 
1.60 
2.00 
2.20 
2.40 
5 
2.10 
2.25 
1.90 
4.00 
4.40 
4.70 
3.70 
1.90 
1.60 
2.00 
2.20 
2.30 
6 
2.10 
2.15 
1.90 
4.20 
4.30 
4.60 
3.60 
1.90 
1.60 
2.00 
2.20 
2.30 
7 
2.10 
2.20 
1.80 
4.20 
4.30 
4.50 
3.50 
1.80 
1.70 
1.90 
2.20 
2.20 
8 
2.10 
2.30 
1.70 
4.10 
4.30 
4.60 
3.50 
1.80 
1.70 
1.90 
2.10 
2.20 
9 
2.00 
2.20 
1.70 
3.90 
4.40 
4.60 
3.30 
1.80 
1.70 
1.90 
2.10 
2.20 
10 
2.00 
2.20 
1.80 
3.90 
4.40 
4.70 
3.10 
1. 70 
1.70 
1.90 
2.10 
2.20 
11 
2.10 
2.00 
1.80 
4.10 
4.50 
4.90 
3.00 
1.70 
1.70 
2.00 
2.10 
2.20 
12 
2.10 
1.90 
1.80 
4.20 
4.70 
4.90 
2.90 
1.60 
1.70 
2.00 
2.10 
2.30 
13 
2.00 
1.90 
1.90 
4.30 
4.80 
5.00 
2.80 
1.60 
1.70 
2.00 
2,00 
2.30 
14 
2.00 
1.85 
1.90 
4.30 
4.90 
5.00 
2.70 
1.60 
1.70 
2.00 
2.00 
2.30 
15 
2.00 
1.80 
2.00 
4.30 
5.15 
5.10 
2.70 
1.70 
1.70 
2.00 
2.00 
2.30 
16... 
2.00 
2.00 
1.80 
1.90 
2.00 
2.10 
4.15 
4.00 
5.25 
5.40 
5.10 
5.00 
2.60 
2.60 
1.70 
1.70 
1.70 
1.70 
1.90 
1.90 
2.00 
2.00 
2.30 
2.30 
17 
18 
2.00 
1.80 
2.20 
3.85 
5.55 
5.05 
2.50 
1.70 
1.70 
2.00 
2.00 
2.20 
19 
2.10 
1.70 
2.20 
3.80 
5.75 
5.10 
2.50 
1.60 
1.70 
2.00 
2.00 
2.10 
20 
2.10 
1.70 
2.30 
3.80 
5.95 
5.00 
2.40 
1.60 
1.70 
2.00 
2.00 
2.10 
21 
2.10 
1.70 
2.40 
3.70 
6.00 
4.90 
2.40 
1.60 
1.70 
2.00 
2.00 
2.10 
22 
2.00 
1.80 
2.50 
3.70 
6.05 
4.80 
2.40 
1.70 
1.70 
2.00 
2.00 
2.00 
23 
2.00 
1.80 
2.60 
3.75 
5.95 
4.70 
2.30 
1.70 
1.80 
2.00 
2.00 
2.00 
24 
2.00 
1.80 
2.70 
3.75 
5.80 
4.60 
2.30 
1.70 
1.80 
2.00 
2.00 
1.90 
25 
2.00 
1.90 
2.80 
4.00 
5.55 
4.60 
2.30 
1.60 
1.80 
2.00 
2.00 
1.90 
26 
2.10 
1.90 
2.90 
4.10 
5.40 
4.50 
2.20 
1.60 
1.80 
2.00 
2.10 
1.80 
27 
2.10 
1.90 
3.00 
4.15 
5.20 
4.40 
2.20 
1.60 
1.80 
2.10 
2.10 
1.80 
28 
2.10 
1.80 
3.10 
4.30 
4.75 
4.30 
2.10 
1.70 
1.80 
2.10 
2.20 
1.80 
29 
2.05 
3.20 
4.25 
4.65 
4.20 
2.10 
1.60 
1.90 
2.10 
2.30 
1.80 
30 
2.10 
3.30 
4.15 
4.60 
4.10 
2.00 
1.60 
1.90 
2.10 
2.30 
1.80 
31 
2.00 
3.40 
4.60 
2.00 
1.60 
2.10 
1.80 
