Climatic geomorphologists, and eolian geomorphologists in particular, have always been interested in studying dunes to understand and construct past climatic conditions. Smith’s 1965 paper presents an excellent example of a reconnaissance piece of scientific work that set the foundation for (1) using aerial photo-interpretation to provide chronological information about dune fields; (2) the use of eolian processes and landforms as climate change indicators; and (3) extraterrestrial or planetary geomorphology. This article briefly describes Smith’s background, background on Nebraska Sand Hills, and the impact and legacy of Smith’s classic paper.
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