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.