Table 1 Heat flow measurements using the FIELAX probe (11 thermistors*) in the Wagner and Consag basins.
From: High heat flow and ocean acidification at a nascent rift in the northern Gulf of California
Station | Latitude | Longitude | Depth | Sea bottom temperature | Heat flow | Error (%) | ||
---|---|---|---|---|---|---|---|---|
(°N) | (min N) | (°W) | (min W) | (m) | (°C) | (mW m−2) | ||
1 | 30 | 32.807 | 113 | 59.204 | 178 | 15 | 16 | 22.84 |
2 | 31 | 6.653 | 114 | 6.822 | 123 | 18 | 2,907 | 0.01 |
3 | 31 | 3.716 | 114 | 5.183 | 98 | 20 | 7,115 | 0.01 |
4 | 31 | 7.800 | 114 | 12.533 | 116 | 17 | 892 | 0.22 |
5 | 31 | 0.183 | 114 | 16.616 | 97 | 18 | 1,216 | 2.13 |
6 | 30 | 58.800 | 114 | 12.317 | 214 | 15 | 42 | 3.89 |
7 | 31 | 1.200 | 114 | 9.983 | 213 | 15 | 27 | 2.24 |
8 | 30 | 49.500 | 114 | 15.267 | 98 | 19 | 229 | 2.46 |
9 | 30 | 39.768 | 114 | 13.319 | 102 | 18 | 163 | 0.23 |
10 | 30 | 43.310 | 114 | 8.015 | 193 | 14 | 310 | 0.71 |
11 | 30 | 46.034 | 114 | 3.629 | 129 | 16 | 533 | 3.85 |
12 | 30 | 47.993 | 113 | 59.043 | 95 | 28 | 1,369 | 6.97 |
13 | 30 | 50.651 | 113 | 59.988 | 84 | 20 | 1,206 | 0.24 |
13A | 30 | 50.649 | 113 | 59.982 | 83 | 20 | 1,121 | 4.88 |
14† | 31 | 3.701 | 114 | 5.119 | 91 | 27 | 15,436 | 0.84 |
15 | 31 | 3.535 | 114 | 4.628 | 82 | 20 | 1,450 | 2.49 |
16 | 30 | 59.752 | 114 | 3.959 | 95 | 18 | 621 | 0.63 |
17 | 30 | 55.080 | 114 | 2.284 | 91 | 19 | 859 | 0.42 |
18 | 30 | 50.519 | 114 | 0.005 | 88 | 20 | 2,053 | 0.44 |
19 | 30 | 40.634 | 113 | 55.364 | 116 | 17 | 416 | 1.45 |
20 | 30 | 38.904 | 113 | 55.104 | 123 | 16 | 709 | 5.48 |
21 | 30 | 36.824 | 113 | 54.323 | 115 | 17 | 2,559 | 2.24 |