Source-bordering aeolian dune formation along the Scheldt River (southern Netherlands – northern Belgium) was caused by Younger Dryas cooling, high river gradient and southwesterly summer winds

Kasse, Cornelis ; Woolderink, Hessel A.G. ; Kloos, Marjan E. ; Hoek, Wim Z.

Geologie en mijnbouw, 2020, Vol.99, Article e13

Cambridge, UK: Cambridge University Press

Texto completo disponível