Asset Details
Do you wish to reserve the book?
Glacial geomorphology in the Wicklow Mountains, Ireland
Hey, we have placed the reservation for you!
By the way, why not check out events that you can attend while you pick your title.
Oops! Something went wrong.
Looks like we were not able to place the reservation. Kindly try again later.
Are you sure you want to remove the book from the shelf?
Glacial geomorphology in the Wicklow Mountains, Ireland
Do you wish to request the book?
Glacial geomorphology in the Wicklow Mountains, Ireland
Please be aware that the book you have requested cannot be checked out. If you would like to checkout this book, you can reserve another copy
We have requested the book for you!
Your request is successful and it will be processed during the Library working hours. Please check the status of your request in My Requests.
Oops! Something went wrong.
Looks like we were not able to place your request. Kindly try again later.
Journal Article
Glacial geomorphology in the Wicklow Mountains, Ireland
2023
Overview
We present a detailed 1:50,000-scale glacial geomorphological map covering ∼450 km
2
of the Wicklow Mountains, eastern Ireland. The region was glaciated at the Last Glacial Maximum, but little is known about the timing and pattern of deglaciation during the Last Glacial-Interglacial Transition or the extent of glacier regrowth during the Younger Dryas. The absence of detailed glacial geomorphological mapping has been a barrier to understanding these outstanding questions before now. Mapping of the area was compiled during field campaigns supported by the assessment of remotely-sensed imagery. Ice-marginal moraines are the most prevalent landform mapped and these have been classified into three groups based on differences in morphology. Other evidence for glaciation includes glacially-transported boulders, ice-moulded bedrock, meltwater channels, terraces, talus and summit blockfields. The map forms an essential basis for future work that will investigate glacial landsystems, deglaciation patterns and timing, and the style and extent of Younger Dryas glaciation.
