Schmidt-hammer exposure-age dating: a review of principles and practice
JA Matthews, S Winkler - Earth-Science Reviews, 2022 - Elsevier
Schmidt-hammer exposure-age dating (SHD) is a numerical, calibrated-age dating
technique based on the degree of weathering of rock surfaces. The Schmidt hammer …
technique based on the degree of weathering of rock surfaces. The Schmidt hammer …
[HTML][HTML] Origins of the divergent evolution of mountain glaciers during deglaciation: Hofsdalur cirques, Northern Iceland
LM Tanarro, D Palacios… - Quaternary Science …, 2021 - Elsevier
The aim of this work is to study the process of transformation of debris-free mountain glaciers
into debris-covered glaciers and rock glaciers, and to examine the factors driving diverging …
into debris-covered glaciers and rock glaciers, and to examine the factors driving diverging …
Little Ice Age glaciers and climate in the Mediterranean mountains: a new analysis
PD Hughes - Cuadernos de investigación geográfica …, 2018 - dialnet.unirioja.es
Glaciers were common across the Mediterranean mountains during the Little Ice Age. In
parts of Turkey some glaciers were several kilometres longer than they are today, whilst in …
parts of Turkey some glaciers were several kilometres longer than they are today, whilst in …
Determining topographic shielding from digital elevation models for cosmogenic nuclide analysis: a GIS model for discrete sample sites
Y Li - Journal of Mountain Science, 2018 - Springer
Topographic shielding (TS) is an important factor in cosmogenic nuclide surface exposure
dating. The development of geographic information systems (GIS) and the availability of …
dating. The development of geographic information systems (GIS) and the availability of …
Deglaciation of the highest mountains in Scandinavia at the Younger Dryas–Holocene transition: evidence from surface exposure‐age dating of ice‐marginal …
Surface exposure–age dating was applied to rock surfaces associated with ice‐marginal
moraines at elevations of~ 1520–1780 m asl on the slopes of Galdhøpiggen and …
moraines at elevations of~ 1520–1780 m asl on the slopes of Galdhøpiggen and …
Small rock‐slope failures conditioned by Holocene permafrost degradation: a new approach and conceptual model based on Schmidt‐hammer exposure‐age dating …
Rock‐slope failures (RSF s) constitute significant natural hazards, but the geophysical
processes that control their timing are poorly understood. However, robust chronologies can …
processes that control their timing are poorly understood. However, robust chronologies can …
[HTML][HTML] The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: A new study case from the Cantabrian Mountains (Spain)
J Santos-González, RB González-Gutiérrez… - Geomorphology, 2022 - Elsevier
Abstract During the Late Pleistocene, the main mountain ranges of the Iberian Peninsula
were covered by small icefields and cirque and alpine glaciers. The deglaciation triggered …
were covered by small icefields and cirque and alpine glaciers. The deglaciation triggered …
[HTML][HTML] Paleo-glacial reconstruction of the Thajwas glacier in the Kashmir Himalaya using 10Be cosmogenic radionuclide dating
Quantitative glacial chronologies of past glaciations are sparse in the Himalaya, and mostly
absent in the Kashmir Himalaya. We used cosmogenic 10 Be exposure dating, and …
absent in the Kashmir Himalaya. We used cosmogenic 10 Be exposure dating, and …
Schmidt Hammer exposure dating (SHED): Calibration procedures, new exposure age data and an online calculator
Recent research has established Schmidt Hammer exposure dating (SHED) as an effective
method for dating glacial landforms in the UK. This paper presents new data and discussion …
method for dating glacial landforms in the UK. This paper presents new data and discussion …
Rapid age assessment of glacial landforms in the Pyrenees using Schmidt hammer exposure dating (SHED)
Schmidt hammer (SH) sampling of 54 10Be-dated granite surfaces from the Pyrenees
reveals a clear relationship between exposure and weathering through time (n= 52, R2 …
reveals a clear relationship between exposure and weathering through time (n= 52, R2 …