This study investigates the genesis of late Quaternary glacial landforms in the Serra da Peneda Mountains of NW Portugal. Using till macrofabric and grain size analysis, this research tries to identify till types present in moraines and other glacial landforms in order to determine their depositional environment and landform classification. Basically, this research focuses on reconstructing paleo-glacial processes.
Santos, J.A., Santos-González, J. and Redondo-Vega, J.M., 2014. Till Fabric Analysis and Origin of Late Quaternary Moraines in the Serra da Peneda Mountains, NW Portugal. Physical Geography, Vol. 36, 1–18. DOI:10.1080/02723646.2014.961218.
https://www.tandfonline.com/doi/abs/9.1080/02723646.2014.961218/
Santos, J.A., Santos-González, J. and Redondo-Vega, J.M., 2014. Till Fabric Analysis and Origin of Late Quaternary Moraines in the Serra da Peneda Mountains, NW Portugal. Geological Society of America Abstracts with Programs, Northeastern Section (50th) Annual Meeting, March 2015; Vol. 47, No. 3, p. 104.
https://gsa.confex.com/gsa/2015NE/webprogram/Paper251352.html
Santos, J.A., Cunha, L.J., Vieira, A.A. and Bento-Gonçalves, A.J., 2012. Genesis of the Alto Vez Glacial Valley Pleistocene Moraines, Peneda Mountains, Northwest Portugal. Proceedings of the 6th Bi-Annual Conference of the Association of Portuguese Geomorphologists, February 2013; pp. 57–62.