Cosmogenic Cl-36 exposure ages of bedrock and glacially transported boulders, SW Lakes District, England
Please cite: C.K. Ballantyne, J.O. Stone and L.K. Fifield, Glaciation and deglaciation of the SW Lake District, England: implications of cosmogenic Cl-36 exposure dating
Table 1: Input data for cosmogenic Cl-36 exposure age calculations
| Sample name | Latitude | Longitude | Altitude | Top | Bottom | Density | Horizon corr'n | Estimated erosion | [Cl-36] | error | Target CaO | error | Target K2O | error | Target TiO2 | error | Target Fe2O3 | error | Target Cl | error | WR_SiO2 | error | WR_TiO2 | error | WR_Al2O3 | error | WR_Fe2O3 | error | WR_FeO | error | WR_MnO | error | WR_MgO | error | WR_CaO | error | WR_Na2O | error | WR_K2O | error | WR_P2O5 | error | WR_H2O | error | WR_CO2 | error | Li | error | B | error | WR_Cl | error | Cr | error | Sm | error | Gd | error | U | error | Th | error |
| (deg N) | (deg W) | (m) | (cm) | (cm) | (g/cm^3) | (cm) | (atom/g) | (atom/g) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (ppm wt) | (ppm wt) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (wt%) | (rel) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | (ppm wt) | ||
| LD-05 | 54.4532 | -3.2107 | 960 | 0 | 3.0 | 2.65 | 1.000 | 0 | 8009986 | 355292 | 4.84 | 0.01 | 2.88 | 0.01 | 1.32 | 0.01 | 6.35 | 0.01 | 286 | 11 | 60.4 | 0.01 | 1.32 | 0.01 | 15.39 | 0.01 | 6.35 | 0.01 | 0 | 0.01 | 0.17 | 0.01 | 3.81 | 0.01 | 4.84 | 0.01 | 3.23 | 0.01 | 2.88 | 0.01 | 0.06 | 0.01 | 1.65 | 0.05 | 0.1 | 0.05 | 5 | 1 | 34 | 5 | 286 | 11 | 137 | 50 | 5.8 | 0.5 | 5.66 | 0.5 | 2.15 | 0.1 | 7.8 | 0.1 |
| LD-06 | 54.4532 | -3.2107 | 965 | 0 | 3.0 | 2.65 | 1.000 | 0 | 1481642 | 56798 | 7.83 | 0.01 | 1.78 | 0.01 | 1.45 | 0.01 | 10.24 | 0.01 | 24.4 | 0.7 | 54.35 | 0.01 | 1.45 | 0.01 | 13.18 | 0.01 | 10.24 | 0.01 | 0 | 0.01 | 0.3 | 0.01 | 6.87 | 0.01 | 7.83 | 0.01 | 1.55 | 0.01 | 1.78 | 0.01 | 0.04 | 0.01 | 2.25 | 0.05 | 0.1 | 0.05 | 5 | 1 | 39 | 5 | 24.4 | 0.7 | 274 | 50 | 4.9 | 0.5 | 4.97 | 0.5 | 1.63 | 0.1 | 5.6 | 0.1 |
| LD-02 | 54.4517 | -3.2150 | 795 | 0 | 3.0 | 2.65 | 0.990 | 0 | 980173 | 41942 | 1.52 | 0.01 | 3.3 | 0.01 | 0.61 | 0.01 | 3.56 | 0.01 | 35.6 | 1.6 | 68.84 | 0.01 | 0.61 | 0.01 | 14.6 | 0.01 | 3.56 | 0.01 | 0 | 0.01 | 0.1 | 0.01 | 0.76 | 0.01 | 1.52 | 0.01 | 4.37 | 0.01 | 3.3 | 0.01 | 0.01 | 0.01 | 1.1 | 0.05 | 0.1 | 0.05 | 5 | 1 | 5 | 5 | 35.6 | 1.6 | 50 | 50 | 7.8 | 0.5 | 7.17 | 0.5 | 2.33 | 0.1 | 8.2 | 0.1 |
| LD-03 | 54.4504 | -3.2184 | 775 | 0 | 3.0 | 2.65 | 0.963 | 0 | 234293 | 12308 | 2.75 | 0.01 | 1.17 | 0.01 | 0.53 | 0.01 | 3.34 | 0.01 | 36.2 | 0.95 | 70.77 | 0.01 | 0.53 | 0.01 | 15.06 | 0.01 | 3.34 | 0.01 | 0 | 0.01 | 0.11 | 0.01 | 0.28 | 0.01 | 2.75 | 0.01 | 4.8 | 0.01 | 1.17 | 0.01 | 0.01 | 0.01 | 1 | 0.05 | 0.1 | 0.05 | 5 | 1 | 33 | 5 | 36.2 | 0.95 | 50 | 50 | 9.1 | 0.5 | 8.76 | 0.5 | 2.84 | 0.1 | 8.8 | 0.1 |
| LD-07 | 54.4585 | -3.2186 | 765 | 0 | 3.0 | 2.65 | 0.996 | 0 | 95067 | 9272 | 0.96 | 0.01 | 0.62 | 0.01 | 0.48 | 0.01 | 4.28 | 0.01 | 33.9 | 0.7 | 69 | 0.01 | 0.48 | 0.01 | 16.4 | 0.01 | 4.28 | 0.01 | 0 | 0.01 | 0.05 | 0.01 | 0.73 | 0.01 | 0.96 | 0.01 | 7.21 | 0.01 | 0.62 | 0.01 | 0.01 | 0.01 | 1.1 | 0.05 | 0.03 | 0.05 | 5 | 1 | 5 | 5 | 33.9 | 0.7 | 50 | 50 | 8.3 | 0.5 | 7.97 | 0.5 | 3.5 | 0.1 | 15 | 0.1 |
| LD-08 | 54.4594 | -3.2186 | 750 | 0 | 3.0 | 2.65 | 0.996 | 0 | 271337 | 11551 | 0.98 | 0.01 | 4.26 | 0.01 | 0.48 | 0.01 | 2.89 | 0.01 | 31.6 | 0.7 | 71.12 | 0.01 | 0.48 | 0.01 | 15.21 | 0.01 | 2.89 | 0.01 | 0 | 0.01 | 0.08 | 0.01 | 0.48 | 0.01 | 0.98 | 0.01 | 3.53 | 0.01 | 4.26 | 0.01 | 0.03 | 0.01 | 0.9 | 0.05 | 0.1 | 0.05 | 5 | 1 | 24 | 5 | 31.6 | 0.7 | 50 | 50 | 7.2 | 0.5 | 6.92 | 0.5 | 3.12 | 0.1 | 9.5 | 0.1 |
| LD-12 | 54.4433 | -3.3033 | 125 | 0 | 1.5 | 2.70 | 0.971 | 0 | 95393 | 1851 | 4.03 | 0.01 | 0.28 | 0.01 | 0.84 | 0.01 | 4.39 | 0.01 | 38.6 | 0.7 | 64.4 | 0.01 | 0.84 | 0.01 | 16.5 | 0.01 | 4.39 | 0.01 | 0 | 0.01 | 0.05 | 0.01 | 1.29 | 0.01 | 4.03 | 0.01 | 6.06 | 0.01 | 0.28 | 0.01 | 0.01 | 0.01 | 1.35 | 0.05 | 0.1 | 0.05 | 5 | 5 | 5 | 5 | 40 | 20 | 411 | 100 | 4.3 | 0.1 | 4.58 | 0.05 | 2.35 | 0.1 | 6.9 | 0.2 |
| LD-17 | 54.4433 | -3.3033 | 125 | 0 | 3.0 | 2.70 | 0.972 | 0 | 637064 | 9794 | 3.67 | 0.01 | 2.61 | 0.01 | 0.91 | 0.01 | 4.47 | 0.01 | 147.1 | 1.8 | 62.72 | 0.01 | 0.91 | 0.01 | 17.62 | 0.01 | 4.47 | 0.01 | 0 | 0.01 | 0.1 | 0.01 | 1.21 | 0.01 | 3.67 | 0.01 | 5.7 | 0.01 | 2.61 | 0.01 | 0.01 | 0.01 | 0.9 | 0.05 | 0.05 | 0.05 | 5 | 5 | 5 | 5 | 150 | 30 | 274 | 100 | 4.8 | 0.1 | 5.12 | 0.05 | 2.23 | 0.1 | 5.7 | 0.2 |
| LD-09 | 54.4557 | -3.2278 | 595 | 0 | 3.0 | 2.65 | 0.981 | 0 | 396091 | 16330 | 1.15 | 0.01 | 3.25 | 0.01 | 0.44 | 0.01 | 2.93 | 0.01 | 39.4 | 0.6 | 71.22 | 0.01 | 0.44 | 0.01 | 15.05 | 0.01 | 2.93 | 0.01 | 0 | 0.01 | 0.1 | 0.01 | 0.43 | 0.01 | 1.15 | 0.01 | 4.79 | 0.01 | 3.25 | 0.01 | 0.1 | 0.01 | 0.8 | 0.05 | 0.1 | 0.05 | 5 | 1 | 21 | 5 | 39.4 | 0.6 | 50 | 50 | 8.3 | 0.5 | 8.13 | 0.5 | 3.03 | 0.1 | 9.4 | 0.1 |
| LD-10 | 54.4548 | -3.2278 | 595 | 0 | 3.0 | 2.65 | 0.981 | 0 | 202649 | 9033 | 1.31 | 0.01 | 4.52 | 0.01 | 0.42 | 0.01 | 3.65 | 0.01 | 51.8 | 0.8 | 71.54 | 0.01 | 0.42 | 0.01 | 14.22 | 0.01 | 3.65 | 0.01 | 0 | 0.01 | 0.15 | 0.01 | 0.52 | 0.01 | 1.31 | 0.01 | 2.62 | 0.01 | 4.52 | 0.01 | 0.05 | 0.01 | 0.9 | 0.05 | 0.1 | 0.05 | 5 | 1 | 26 | 5 | 51.8 | 0.8 | 50 | 50 | 8.8 | 0.5 | 8.94 | 0.5 | 3.11 | 0.1 | 10.2 | 0.1 |
Table 2: Exposure age results
| Summary | Site and sample data | Results | Target chemical composition | Derived results: correction factors | Derived results: Cl-36 production rates | Cl-36 concentrations | Derived results: Exposure age and limits | ||||||||||||||||||||||||||||||||||||||||||||||
| Sample name | Latitude | Longitude | Altitude | Exposure Age | Min. possible exp. age | [Cl-36] | Target CaO | Target K2O | Target TiO2 | Target Fe2O3 | [Cl] | [Cl] error | Scaling factor (spallation) | Scaling factor (muons) | Thickness correction (spallation) | Thickness correction (thermal n) | Thickness correction (epithermal n) | Horizon correction | Ca spallation rate | error | Ca muon rate | error | K spallation rate | error | K muon rate | error | Ti spallation rate | error | Ti muon rate | error | Fe spallation rate | error | Fe muon rate | error | Cl-35 (thermal n) rate | error | Cl-35 (epithermal n) rate | error | K-39 (n-alpha) rate | error | Cosmogenic Cl-36 prod'n rate | error | Intrinsic n prod'n rate | error | Cosmogenic [Cl-36] | error | Radiogenic [Cl-36] | error | Conventional exposure age | error | internal error | Minimum possible age | error |
| (deg N) | (deg W) | (m) | (kyr) | (kyr) | (10^3 atom/g) | (wt%) | (wt%) | (wt%) | (wt%) | (ppm) | (ppm) | (atom/g/yr) | (atom/g/yr) | (atom/g/yr) | (atom/g/yr) | (atom/g/yr) | (atom/g/yr) | (atom/g/yr) | (atom/g/yr) | (atom/g/yr) | (atom/g/yr) | (atom/g/yr) | (atom/g/yr) | (atom/g/yr) | (atom/g) | (atom/g) | (yr) | (yr) | |||||||||||||||||||||||||
| Samples from above the inferred weathering limit: Scafell Pike summit tor | |||||||||||||||||||||||||||||||||||||||||||||||||||||
| LD-05 | 54.4532 | -3.2107 | 960 | 327.7 ± 36.6 | 279 ± 31.2 | 8010 ± 355 | 4.84 | 2.88 | 1.32 | 6.35 | 286 | 11 | 2.479 | 1.611 | 0.976 | 1.208 | 1.055 | 1.000 | 4.080 | 0.142 | 0.267 | 0.052 | 9.314 | 0.523 | 0.392 | 0.049 | 0.096 | 0.048 | 0.001 | 0.001 | 0.204 | 0.020 | 0.001 | 0.001 | 14.887 | 1.794 | 2.303 | 0.205 | 0.139 | 0.009 | 34.51 | 2.07 | 0.16 | 0.01 | 7938714.1 | 355310.7 | 71271.4 | 3627.9 | 327687.3 | 36603.8 | 21900.2 | 279006.5 | 31166.0 |
| LD-06 | 54.4532 | -3.2107 | 965 | 109.8 ± 6 | 109.8 ± 6 | 1482 ± 57 | 7.83 | 1.78 | 1.45 | 10.24 | 24.4 | 0.7 | 2.490 | 1.615 | 0.976 | 1.227 | 1.031 | 1.000 | 6.628 | 0.231 | 0.434 | 0.085 | 5.781 | 0.326 | 0.243 | 0.030 | 0.106 | 0.053 | 0.001 | 0.001 | 0.331 | 0.033 | 0.002 | 0.002 | 1.235 | 0.141 | 0.168 | 0.014 | 0.083 | 0.005 | 15.24 | 0.44 | 0.01 | 0.00 | 1477716.1 | 56798.0 | 3925.5 | 173.5 | 109761.2 | 5997.9 | 4800.0 | 109761.2 | 5997.9 |
| High-level samples below the inferred weathering limit: Broad Stand bedrock slabs | |||||||||||||||||||||||||||||||||||||||||||||||||||||
| LD-02 | 54.4517 | -3.2150 | 795 | 76.45 ± 5.2 | 76.19 ± 5.19 | 980 ± 42 | 1.52 | 3.3 | 0.61 | 3.56 | 35.6 | 1.6 | 2.155 | 1.495 | 0.976 | 1.189 | 1.080 | 0.990 | 1.103 | 0.039 | 0.077 | 0.015 | 9.186 | 0.516 | 0.413 | 0.051 | 0.038 | 0.019 | 0.000 | 0.000 | 0.099 | 0.010 | 0.001 | 0.001 | 1.969 | 0.301 | 0.305 | 0.030 | 0.169 | 0.011 | 13.79 | 0.62 | 0.03 | 0.00 | 966507.9 | 41949.7 | 13664.7 | 778.5 | 76448.2 | 5203.8 | 3628.1 | 76191.4 | 5186.3 |
| LD-03 | 54.4504 | -3.2184 | 775 | 29.23 ± 2.07 | 28.55 ± 2.02 | 234 ± 12 | 2.75 | 1.17 | 0.53 | 3.34 | 36.2 | 0.95 | 2.118 | 1.481 | 0.976 | 1.185 | 1.083 | 0.963 | 1.908 | 0.067 | 0.135 | 0.026 | 3.114 | 0.177 | 0.141 | 0.018 | 0.032 | 0.016 | 0.000 | 0.000 | 0.088 | 0.009 | 0.001 | 0.001 | 1.684 | 0.216 | 0.303 | 0.026 | 0.050 | 0.003 | 7.82 | 0.31 | 0.03 | 0.00 | 221010.6 | 12321.3 | 13282.4 | 577.4 | 29235.0 | 2067.5 | 1686.0 | 28548.3 | 2018.9 |
| High-level samples below the inferred weathering limit: Lingmell col ice-moulded bedrock | |||||||||||||||||||||||||||||||||||||||||||||||||||||
| LD-07 | 54.4585 | -3.2186 | 765 | 13.18 ± 2.02 | 11.95 ± 1.83 | 95.1 ± 9.3 | 0.96 | 0.62 | 0.48 | 4.28 | 33.9 | 0.7 | 2.100 | 1.474 | 0.976 | 1.194 | 1.081 | 0.996 | 0.682 | 0.025 | 0.048 | 0.009 | 1.691 | 0.099 | 0.077 | 0.010 | 0.029 | 0.015 | 0.000 | 0.000 | 0.116 | 0.012 | 0.001 | 0.001 | 1.888 | 0.294 | 0.282 | 0.025 | 0.032 | 0.002 | 5.27 | 0.34 | 0.06 | 0.00 | 68409.9 | 9350.3 | 26657.0 | 1204.5 | 13183.6 | 2020.3 | 1829.6 | 11945.9 | 1830.6 |
| LD-08 | 54.4594 | -3.2186 | 750 | 17.33 ± 1.13 | 17.33 ± 1.13 | 271 ± 12 | 0.98 | 4.26 | 0.48 | 2.89 | 31.6 | 0.7 | 2.073 | 1.464 | 0.976 | 1.180 | 1.088 | 0.996 | 0.688 | 0.025 | 0.049 | 0.010 | 11.469 | 0.644 | 0.525 | 0.065 | 0.029 | 0.015 | 0.000 | 0.000 | 0.077 | 0.008 | 0.001 | 0.001 | 1.540 | 0.202 | 0.282 | 0.024 | 0.192 | 0.012 | 15.19 | 0.69 | 0.03 | 0.00 | 258059.0 | 11562.8 | 13277.6 | 518.2 | 17332.6 | 1125.6 | 792.3 | 17332.6 | 1125.6 |
| Low level samples from a valley-floor roches moutonnŽe, Wasdale | |||||||||||||||||||||||||||||||||||||||||||||||||||||
| LD-12 | 54.4433 | -3.3033 | 125 | 19.95 ± 1.35 | 18.05 ± 1.22 | 95.4 ± 1.9 | 4.03 | 0.28 | 0.84 | 4.39 | 38.6 | 0.7 | 1.164 | 1.089 | 0.987 | 1.107 | 1.042 | 0.971 | 1.569 | 0.055 | 0.146 | 0.029 | 0.418 | 0.028 | 0.025 | 0.003 | 0.028 | 0.014 | 0.000 | 0.000 | 0.065 | 0.007 | 0.001 | 0.001 | 1.222 | 0.205 | 0.164 | 0.015 | 0.008 | 0.001 | 4.03 | 0.25 | 0.04 | 0.00 | 78567.9 | 2036.6 | 16825.0 | 848.4 | 19952.7 | 1351.9 | 529.3 | 18052.4 | 1223.1 |
| LD-17 | 54.4433 | -3.3033 | 125 | 50.03 ± 3.47 | 44.93 ± 3.12 | 637 ± 10 | 3.67 | 2.61 | 0.91 | 4.47 | 147.1 | 1.8 | 1.164 | 1.089 | 0.975 | 1.185 | 1.091 | 0.972 | 1.412 | 0.049 | 0.133 | 0.026 | 3.852 | 0.217 | 0.233 | 0.029 | 0.030 | 0.015 | 0.000 | 0.000 | 0.066 | 0.007 | 0.001 | 0.001 | 4.573 | 0.644 | 0.769 | 0.064 | 0.075 | 0.005 | 12.42 | 0.79 | 0.12 | 0.01 | 587041.4 | 10056.5 | 50022.6 | 2283.2 | 50033.4 | 3474.4 | 908.4 | 44928.4 | 3119.9 |
| Samples from glacially-transported boulders inside the limit of later corrie glaciation | |||||||||||||||||||||||||||||||||||||||||||||||||||||
| LD-09 | 54.4557 | -3.2278 | 595 | 35.11 ± 2.25 | 34.97 ± 2.24 | 396 ± 16 | 1.15 | 3.25 | 0.44 | 2.93 | 39.4 | 0.6 | 1.810 | 1.363 | 0.976 | 1.177 | 1.093 | 0.981 | 0.694 | 0.025 | 0.053 | 0.010 | 7.528 | 0.423 | 0.367 | 0.046 | 0.023 | 0.011 | 0.000 | 0.000 | 0.068 | 0.007 | 0.001 | 0.001 | 1.672 | 0.218 | 0.319 | 0.027 | 0.128 | 0.008 | 11.24 | 0.49 | 0.04 | 0.00 | 379030.3 | 16342.8 | 17060.8 | 644.5 | 35110.1 | 2250.3 | 1576.7 | 34973.2 | 2241.5 |
| LD-10 | 54.4548 | -3.2278 | 595 | 12.47 ± 0.83 | 12.45 ± 0.83 | 203 ± 9 | 1.31 | 4.52 | 0.42 | 3.65 | 51.8 | 0.8 | 1.810 | 1.363 | 0.976 | 1.179 | 1.088 | 0.981 | 0.791 | 0.028 | 0.060 | 0.012 | 10.470 | 0.588 | 0.511 | 0.064 | 0.022 | 0.011 | 0.000 | 0.000 | 0.084 | 0.008 | 0.001 | 0.001 | 2.052 | 0.245 | 0.402 | 0.033 | 0.166 | 0.011 | 15.02 | 0.66 | 0.04 | 0.00 | 184631.3 | 9054.7 | 18017.4 | 630.6 | 12471.3 | 831.1 | 620.5 | 12450.6 | 829.7 |