GPS and Isotopic Data for Potomac River Samples used in Science Paper | ||||||||||
Sample | Description * | Elevation | Easting | Northing | 10Be activity | Model Age | ||||
ID | (masl) | (m) | (m) | (104 atoms g-1) | (ky) ¤ | |||||
GF-21 | PS/CHT | 42 | 305651 | 4316940 | 17.8 | ± | 0.6 | 37.1 | ± | 3.9 |
GF-29 | PS | 39 | 305478 | 4317077 | 17.8 | ± | 0.7 | 38.1 | ± | 4.1 |
GF-32 | PS | 44 | 305331 | 4317611 | 18.8 | ± | 0.7 | 38.8 | ± | 4.2 |
GF-33 | PS | 47 | 304998 | 4318280 | 15.6 | ± | 0.5 | 32.4 | ± | 3.4 |
GF-40 | PS | 46 | 305164 | 4318186 | 18.2 | ± | 0.6 | 37.5 | ± | 4.0 |
GF-65 | PS/GFT | 43 | 304964 | 4318557 | 12.9 | ± | 0.4 | 26.5 | ± | 2.8 |
GF-37 | PS | 44 | 304792 | 4318599 | 12.5 | ± | 0.5 | 25.5 | ± | 2.7 |
GF-37X | PS | 44 | 304792 | 4318599 | 12.7 | ± | 0.5 | 25.9 | ± | 2.8 |
GF-46 | PS | 47 | 304991 | 4318736 | 14.9 | ± | 0.5 | 30.2 | ± | 3.2 |
GF-42 | High PS | 47 | 305258 | 4317839 | 26.8 | ± | 0.9 | 55.7 | ± | 5.9 |
GF-43 | High PS | 47 | 305230 | 4317859 | 25.6 | ± | 0.8 | 52.9 | ± | 5.6 |
GF-31 | High PS | 47 | 305394 | 4317349 | 37.5 | ± | 1.1 | 77.9 | ± | 8.3 |
GF-35 | High PS | 45 | 305372 | 4317142 | 36.8 | ± | 1.2 | 76.3 | ± | 8.1 |
GF-38 | High PS | 49 | 304740 | 4318427 | 41.7 | ± | 1.3 | 85.6 | ± | 9.2 |
GF-39 | High PS | 51 | 304765 | 4318443 | 30.3 | ± | 0.9 | 61.7 | ± | 6.5 |
GF-22 | CHT | 39 | 305663 | 4316947 | 11.6 | ± | 0.4 | 27.7 | ± | 3.0 |
GF-23 | CHT | 34 | 305664 | 4316954 | 9.37 | ± | 0.3 | 22.8 | ± | 2.4 |
GF-25 | CHT | 32 | 305681 | 4316952 | 8.88 | ± | 0.4 | 20.0 | ± | 2.2 |
GF-27 | CHT | 25 | 305674 | 4316965 | 7.59 | ± | 0.3 | 16.9 | ± | 1.9 |
GF-28 | CHT | 24 | 305650 | 4316970 | 5.82 | ± | 0.3 | 12.7 | ± | 1.5 |
GF-66 | GFT | 39 | 304941 | 4318549 | 7.59 | ± | 0.3 | 15.5 | ± | 1.7 |
GF-67 | GFT | 34 | 304932 | 4318542 | 3.72 | ± | 0.2 | 7.6 | ± | 0.8 |
* Abrieviations in the description field indicate from what part of Mather Gorge the samples were collected and/or what kind of analysis they were used for. PS=prominent strath level, High PS=moderately weathered high points on the prominent strath level, CHT=lower gorge (Cowhoof Rock) vertical transect, and GFT=Great Falls vertical transect. GF-37x is an independently processed and measured laboratory replicate of GF-37. ¤ Age uncertainties include propagated analytic errors (1 sigma) in carrier addition and AMS measurement, and +/-10% (1 sigma) uncertainty in 10-Be production rate. | ||||||||||