Results 141 to 150 of about 4,101 (225)

Shaping pre-modern digital terrain models: The former topography at Charlemagne's canal construction site. [PDF]

PLoS One, 2018
Schmidt J, Werther L, Zielhofer C.
europepmc   +1 more source

Nanoscale silicate melt textures determine volcanic ash surface chemistry. [PDF]

Nat Commun
Hornby AJ, Ayris PM, Damby DE, Diplas S, Eychenne J, Kendrick JE, Cimarelli C, Kueppers U, Scheu B, Utley JEP, Dingwell DB.   +10 more
europepmc   +1 more source

Rampart

openaire   +1 more source

Perspectives and Challenges of Telemedicine and Artificial Intelligence in Pediatric Dermatology. [PDF]

Children (Basel)
Zama D, Borghesi A, Ranieri A, Manieri E, Pierantoni L, Andreozzi L, Dondi A, Neri I, Lanari M, Calegari R.   +9 more
europepmc   +1 more source

Stones for the rampart

, 2010
openaire   +1 more source

Pronival ramparts

Progress in Physical Geography, 2016
Pronival ramparts are debris ridges formed at the downslope margins of perennial or semi-permanent snowbeds beneath bedrock cliffs. These landforms, also previously known as protalus ramparts, are located in periglacial environments, but the apparent simplicity of rampart formation made these landforms far less interesting than other modified forms of
David William Hedding
exaly   +5 more sources

Landform transitions from pronival ramparts to moraines and rock glaciers: a case study from the Smørbotn cirque, Romsdalsalpane, southern Norway

Geografiska Annaler, Series A: Physical Geography, 2017
John A Matthews, Peter Wilson, Richard W Mourne   +2 more
exaly   +2 more sources

Rock glaciers, protalus ramparts and pronival ramparts in the south-eastern Alps

Geomorphology, 2016
Rock glaciers and protalus ramparts are characteristic landforms of the periglacial domain often used as markers for the occurrence of permafrost in mountain terrains. As such, relict rock glaciers can be used for paleoclimate reconstructions. We present
Renato R Colucci, Chiara Boccali, Manja Zebre   +2 more
exaly   +2 more sources