Morgan, Paul; Blackwell, David D; Spafford, Robert E; Smith, Robert B (1977): Component parts of the World Heat Flow Data Collection [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.807412
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
International Heat Flow Commission, I H F C (2012): Global Heat Flow Database. The Global Heat Flow Database of the International Heat Flow Commission (IHFC), University of North Dakota, USA; (data copied, 2012-10), https://ihfc-iugg.org/products/global-heat-flow-database/data
Morgan, Paul; Blackwell, David D; Spafford, Robert E; Smith, Robert B (1977): Heat flow measurements in Yellowstone Lake and the thermal structure of the Yellowstone Caldera. Journal of Geophysical Research, 82(26), 3719-3932, https://doi.org/10.1029/JB082i026p03719
Further details:
Jessop, Alan M; Hobart, Michael A; Sclater, John G (1976): The World Heat Flow Data Collection - 1975. Geological Survey of Canada, Earth Physics Branch, Geothermal Series, 5, 10 pp, hdl:10013/epic.40176.d002
Coverage:
Median Latitude: 44.449932 * Median Longitude: -110.368268 * South-bound Latitude: 44.330000 * West-bound Longitude: -110.541700 * North-bound Latitude: 44.550000 * East-bound Longitude: -110.245000
Minimum ELEVATION: -92 m a.s.l. * Maximum ELEVATION: -21 m a.s.l.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Area/locality | Area | Morgan, Paul | |||
2 | Sample, optional label/labor no | Lab no | Morgan, Paul | |||
3 | LATITUDE | Latitude | Geocode | |||
4 | LONGITUDE | Longitude | Geocode | |||
5 | ELEVATION | Elevation | m a.s.l. | Geocode | ||
6 | Depth, bottom/max | Depth bot | m | Morgan, Paul | Maximum depth | |
7 | Temperature gradient | T grad | mK/m | Morgan, Paul | ||
8 | Number of conductivity measurements | No Cond | Morgan, Paul | |||
9 | Conductivity, average | Cond average | W/m K | Morgan, Paul | ||
10 | Heat flow | HF | mW/m2 | Morgan, Paul | ||
11 | Number | No | Morgan, Paul | Number of individual sites |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
162 data points
Data
1 Area | 2 Lab no | 3 Latitude | 4 Longitude | 5 Elevation [m a.s.l.] | 6 Depth bot [m] | 7 T grad [mK/m] | 8 No Cond | 9 Cond average [W/m K] | 10 HF [mW/m2] | 11 No |
---|---|---|---|---|---|---|---|---|---|---|
US3069 | YNP-ST3 | 44.5500 | -110.3117 | -27 | 4 | 20420 | 0.75 | 15300 | 1 | |
US3071 | YNP-ST4 | 44.5433 | -110.3117 | -21 | 4 | 2165 | 0.75 | 1620 | 1 | |
US3072 | YNP-ST2 | 44.5400 | -110.3833 | -58 | 4 | 440 | 0.96 | 420 | 1 | |
US3073 | YNP-ST1 | 44.5383 | -110.3900 | -59 | 4 | 630 | 0.96 | 600 | 1 | |
US3075 | YNP-ST18 | 44.5117 | -110.3650 | -73 | 5 | 6660 | 3 | 0.78 | 500 | 1 |
US3076 | YNP-ST5 | 44.5000 | -110.3217 | -90 | 4 | 860 | 0.75 | 645 | 1 | |
US3080 | YNP-ST6 | 44.4817 | -110.3417 | -90 | 5 | 640 | 0.75 | 480 | 1 | |
US3081 | YNP-ST22 | 44.4667 | -110.3833 | -82 | 5 | 885 | 0.75 | 665 | 1 | |
US3082 | YNP-ST17 | 44.4650 | -110.3317 | -84 | 5 | 505 | 1 | 0.75 | 380 | 1 |
US3083 | YNP-ST10 | 44.4583 | -110.4383 | -53 | 5 | 860 | 0.75 | 645 | 1 | |
US3084 | YNP-ST20 | 44.4533 | -110.4667 | -46 | 4 | 910 | 4 | 0.78 | 680 | 1 |
US3085 | YNP-ST19 | 44.4417 | -110.5067 | -37 | 5 | 1100 | 0.75 | 825 | 1 | |
US3086 | YNP-ST16 | 44.4400 | -110.3167 | -79 | 5 | 160 | 1 | 0.75 | 120 | 1 |
US3087 | YNP-ST21 | 44.4333 | -110.4000 | -82 | 5 | 255 | 4 | 0.75 | 190 | 1 |
US3088 | YNP-ST11 | 44.4317 | -110.5350 | -92 | 5 | 1835 | 0.75 | 1375 | 1 | |
US3089 | YNP-ST15 | 44.4217 | -110.3167 | -80 | 5 | 160 | 0.75 | 120 | 1 | |
US3091 | YNP-ST12 | 44.4117 | -110.5417 | -84 | 5 | 2110 | 4 | 0.74 | 1580 | 1 |
US3092 | YNP-ST9 | 44.4067 | -110.2867 | -82 | 5 | 130 | 0.75 | 98 | 1 | |
US3093 | YNP-ST13 | 44.3800 | -110.3267 | -53 | 5 | 330 | 4 | 0.75 | 250 | 1 |
US3097 | YNP-ST8 | 44.3617 | -110.2483 | -82 | 4 | 120 | 0.75 | 90 | 1 | |
US3098 | YNP-ST14 | 44.3317 | -110.3333 | -61 | 5 | 245 | 0.75 | 185 | 1 | |
US3099 | YNP-ST7 | 44.3300 | -110.2450 | -76 | 4 | 130 | 1 | 0.75 | 98 | 1 |