Ice wastage in Glenmore, upper Spey valley, Inverness-shire | Semantic Scholar
Kame - Wikipedia
Kame terrace | geology | Britannica
Glen Roy and Glen Spean | SpringerLink
A variety of landforms are associated with melt water from glaciers, including Outwash plains or Sandur, Varves, Braided Streams, Eskers, Kames and Kame terraces, Kettle holes and proglacial lakes.
Glacier dynamics during a phase of Late Quaternary warming in Patagonia reconstructed from sediment-landform associations - ScienceDirect
The Last Glaciers In Glenshee - Cateran Ecomuseum
The Glen Einich delta, viewed from the moraine of the Glenmore lobe.... | Download Scientific Diagram
The Glacial Geomorphology Around Inverness and the Great Glen | SpringerLink
Theoretical model of formation of glaciolacustrine kame terrace. (1)... | Download Scientific Diagram
Kame terrace | geology | Britannica
The Last Glaciers In Glenshee - Cateran Ecomuseum
Kame terraces along the northern margin of Kvíárjökull: a) view from... | Download Scientific Diagram
Phys-Geog: Fluvioglacial landforms: Formaton of Kames and Eskers 2
Late readvance and rapid final deglaciation of the last ice sheet in the Grampian Mountains, Scotland - Hall - 2016 - Journal of Quaternary Science - Wiley Online Library
Lateglacial and early Holocene evolution of the Tyne Valley in response to climatic shifts and possible paraglacial landscape legacies - ScienceDirect
River Systems and Fluvial Landforms - Geology (U.S. National Park Service)
A series of kame terraces along the southern flank of the Findelen... | Download Scientific Diagram
Meltwater channels and deposits | NatureScot
GCR Series No. 6. Quaternary of Scotland: Chapter 9 (Eastern Grampian Mountains)
Geomorphological features within Glen Turret: (A) Lateral moraines on... | Download Scientific Diagram
My partner just returned from a trip to the lovely land and there where multiple pictures of hills and hillsides that looked like this. From what they gathered, they believe it's from
The Last Glaciers In Glenshee - Cateran Ecomuseum
http://eprints.gla.ac.uk/144740/
