Timing of glacial retreat in the Wicklow Mountains, Ireland, conditioned by glacier size and topography

@article{Tomkins2018TimingOG,
  title={Timing of glacial retreat in the Wicklow Mountains, Ireland, conditioned by glacier size and topography},
  author={Matt D. Tomkins and Jason M. Dortch and Philip D. Hughes and Jonny J. Huck and Toby N. Tonkin and Iestyn D. Barr},
  journal={Journal of Quaternary Science},
  year={2018},
  volume={33}
}
Reconstructing the deglacial history of palaeo‐glaciers provides vital information on retreat processes, information which can inform predictions of the future behaviour of many of the world's glaciers. On this basis, this paper presents 170 Schmidt Hammer exposure ages from moraine boulders and glacially sculpted bedrock to reveal the post‐Last Glacial Maximum (LGM) history of the Wicklow Mountains, Ireland. These data suggest that large ice masses survived for 4–7 ka after retreat of the… 
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Cryospheric Geomorphology: Dating Glacial Landforms I: Archival, Incremental, Relative Dating Techniques and Age-Equivalent Stratigraphic Markers
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Age determination of glacially-transported boulders in Ireland and Scotland using Schmidt-hammer exposure-age dating (SHD) and terrestrial cosmogenic nuclide (TCN) exposure-age dating
Abstract Schmidt-hammer exposure-age dating (SHD) was applied at 15 sites with glacially-transported granite boulders in parts of northern and western Ireland and southwest Scotland that had been
Small rock‐slope failures conditioned by Holocene permafrost degradation: a new approach and conceptual model based on Schmidt‐hammer exposure‐age dating, Jotunheimen, southern Norway
Rock‐slope failures (RSFs) constitute significant natural hazards, but the geophysical processes that control their timing are poorly understood. However, robust chronologies can provide valuable
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Recalibration of published Be ages from the classic cirque moraines at Keskadale, Lake District, in combination with calibrated relative ages provided by Schmidt hammer exposure dating (SHED) in the

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