| PART I. SAMPLE LOCATIONS AND EXPOSURE AGES, MARTHA'S VINEYARD AND CAPE COD, MASSACHUSETTS | |||||||||
| Please cite: | |||||||||
| Balco G., Stone J.O., Porter S.C., Caffee M. Cosmogenic-nuclide ages for New England coastal moraines, Martha's Vineyard and Cape Cod, Massachusetts, USA. Quaternary Science Reviews 21, 2127-2135 (2002). | |||||||||
| in reference to these data. | |||||||||
| Part II of this table shows production rate scaling factors used to calculate these exposure ages. | |||||||||
| Sample | N latitude | W longitude | Elevation | [10Be ]1 | 10Be age (yr)2 | [26Al]1 | 26Al age (yr)2 | 26Al/10Be | Mean of Al and Be ages |
| (DD) | (DD) | (m) | (104 atoms/g) | and 1 std. error3 | (104 atoms/g) | and 1 std. error3 | ratio | (yr) and 1 std. error3 | |
| Martha's Vineyard Moraine | |||||||||
| PH-1 | 41.3567 | 70.7348 | 91 | 12.35 ± 0.37 | 24400 ± 1700 | 71.24 ± 3.12 | 23400 ± 1800 | 5.8 ± 0.3 | 24000 ± 1200 |
| WR-2 | 41.3937 | 70.6992 | 54 | 12.29 ± 0.36 | 24700 ± 1700 | 74.91 ± 4.22 | 25000 ± 2100 | 6.1 ± 0.4 | 24800 ± 1300 |
| WR-3 | 41.3922 | 70.6995 | 54 | 12.28 ± 0.47 | 24500 ± 1800 | 60.44 ± 17.58 | 20100 ± 6100 | 4.9 ± 1.4 | 24200 ± 1700 |
| WR-4 | 41.3939 | 70.6972 | 30 | 12.18 ± 0.35 | 25300 ± 1700 | 70.7 ± 2.96 | 24400 ± 1800 | 5.8 ± 0.3 | 24900 ± 1200 |
| WR-5 | 41.3920 | 70.6983 | 51 | 10.29 ± 0.3 | 21500 ± 1400 | 61.19 ± 2.95 | 21200 ± 1700 | 5.9 ± 0.3 | 21400 ± 1100 |
| WR-6 | 41.3897 | 70.7017 | 51 | 11.06 ± 0.42 | 22700 ± 1600 | 65.12 ± 2.56 | 22200 ± 1600 | 5.9 ± 0.3 | 22400 ± 1100 |
| MV 2-27-1 | 41.3483 | 70.7063 | 9 | 14.05 ± 0.36 | 29400 ± 1900 | 92.55 ± 3.71 | 32300 ± 2400 | 6.6 ± 0.3 | 30600 ± 1500 |
| MV 2-27-2 | 41.3633 | 70.7258 | 69 | 28.25 ± 0.7 | 56900 ± 3800 | 162.78 ± 14.06 | 55200 ± 6200 | 5.8 ± 0.5 | 56400 ± 3200 |
| MV 2-27-3 | 41.3483 | 70.7482 | 30 | 10.68 ± 0.28 | 22100 ± 1500 | 63.61 ± 4.08 | 21800 ± 1900 | 6 ± 0.4 | 22000 ± 1200 |
| MV 2-27-4 | 41.3350 | 70.7977 | 33 | 7.55 ± 0.32 | 15700 ± 1100 | 45.77 ± 2.27 | 15700 ± 1200 | 6.1 ± 0.4 | 15700 ± 800 |
| MV 3-07-1 | 41.3758 | 70.7320 | 51 | n.m. | - | 70.72 ± 2.43 | 23800 ± 1700 | - | 23800 ± 1700 |
| MV 3-07-2 | 41.3758 | 70.7320 | 54 | 24.6 ± 0.61 | 49700 ± 3300 | 143.29 ± 7.6 | 48600 ± 4100 | 5.8 ± 0.3 | 49200 ± 2600 |
| MV 3-07-3 | 41.3417 | 70.8143 | 51 | 9.71 ± 0.36 | 19800 ± 1400 | 56.41 ± 3.35 | 19100 ± 1600 | 5.8 ± 0.4 | 19500 ± 1100 |
| Buzzards Bay Moraine | |||||||||
| BB 2-21-1 | 41.5500 | 70.6495 | 12 | 7.98 ± 0.33 | 16700 ± 1200 | 48.39 ± 2.98 | 16800 ± 1500 | 6.1 ± 0.4 | 16700 ± 900 |
| BB 2-24-1 | 41.5317 | 70.6588 | 24 | 8.82 ± 0.31 | 18400 ± 1300 | 52.6 ± 2.33 | 18100 ± 1400 | 6 ± 0.3 | 18200 ± 900 |
| BB 2-24-2 | 41.5317 | 70.6597 | 24 | 8.45 ± 0.34 | 17600 ± 1300 | 54.13 ± 2.48 | 18600 ± 1400 | 6.4 ± 0.4 | 18100 ± 900 |
| BB 2-29-1 | 41.5567 | 70.6458 | 24 | 9.29 ± 0.41 | 19300 ± 1400 | 57.01 ± 2.05 | 19600 ± 1400 | 6.1 ± 0.3 | 19500 ± 1000 |
| BB 2-29-2 | 41.5567 | 70.6458 | 24 | 8.83 ± 0.62 | 18400 ± 1700 | 59.23 ± 11.31 | 20400 ± 4200 | 6.7 ± 1.4 | 18700 ± 1600 |
| BB 3-06-1 | 41.5750 | 70.6178 | 24 | 8.92 ± 0.29 | 18600 ± 1300 | 66.16 ± 5.8 | 22800 ± 2500 | 7.4 ± 0.7 | 19500 ± 1100 |
| BB 3-06-2 | 41.5783 | 70.6192 | 21 | 9.46 ± 0.32 | 19800 ± 1400 | 62.25 ± 3.25 | 21600 ± 1700 | 6.6 ± 0.4 | 20500 ± 1100 |
| BB 3-06-3 | 41.5817 | 70.6217 | 21 | 9.21 ± 0.4 | 19300 ± 1400 | 59.7 ± 4.98 | 20700 ± 2200 | 6.5 ± 0.6 | 19700 ± 1200 |
| BB 3-12-1 | 41.5250 | 70.6532 | 9 | 8.25 ± 0.41 | 17400 ± 1400 | 53.08 ± 3.71 | 18500 ± 1700 | 6.4 ± 0.6 | 17800 ± 1100 |
| BB 3-12-2 | 41.5242 | 70.6528 | 18 | 9.38 ± 0.46 | 19600 ± 1500 | 60.08 ± 2.28 | 20800 ± 1500 | 6.4 ± 0.4 | 20200 ± 1100 |
| 1 Measured relative to LLNL internal standards. Procedural blanks contained 2.4 ± 1.8 x 104 atoms 10Be and <105 atoms 26Al. ±1-standard-error uncertainties are shown and include all known sources of analytical error. | |||||||||
| 2 Ages calculated using production rates of 5.1 ± 0.3 (10Be) and 31.1 ± 0.8 (26Al) at/g SiO2/yr at 1013.25 mb and latitude > 60¡. Ages include a correction for paleomagnetic variation as described in the text. The scaling factors used are tabulated in Part II of this table.. | |||||||||
| 3 Uncertainties include the production rate uncertainty for purposes of comparing individual exposure ages to geologic events dated by other methods. For comparison between exposure ages, only the analytical uncertainties should be taken into account. | |||||||||