Sedimentary evidence of glacial entrainment at Patriot Hills and Union Glacier moraines, Ellsworth Mountains, West Antarctica

• Published in: Anais da Academia Brasileira de Ciências
• Main Authors: VANESSA COSTA, KÁTIA K. ROSA, ALLAN SANDES, CAROLINE DELPUPO, ROSEMARY VIEIRA
• Format: Article in Journal/Newspaper
• Language: English
• Published: Academia Brasileira de Ciências 2022
• Subjects: Antarctica; Ellsworth Mountains; sedimentology; geochemistry; glacial geomorphology; Science; Q; Independence Hills; Patriot Hills; Rossman; Union Glacier; West Antarctica; Antarc*
• Online Access: https://doi.org/10.1590/0001-3765202220210114; https://doaj.org/article/a40d24bc32654136ad77ec00cf891742

Abstract This work aims to analyze and compare the sedimentological data of Ellsworth Mountains, West Antarctica: Patriot/Independence Hills and Union Glacier, and how sedimentological data can be used to infer sediment entrainment. Particular attention was concentrated on morainic deposits. Remote sensing data was used in the identification of deposits and the ice flow; granulometric, morphoscopic, and geochemical analyses were applied to investigate the sedimentary origin and transport history. Sediment rich in Si Al, Fe, and Ca predominate in Independence Hills and Rossman Cove but Ca prevails in Elephant Head. CIA indicated low values, which depict low chemical weathering processes. X-ray diffraction reveals the presence of minerals that constitute the local rocks in the Union Glacier area, and from the unexposed basement rocks in Independence Hills. Principal Component Analysis and Cluster Analysis results suggest the sediment is related to the local rocks in the Union Glacier and distinct exotic sources in Independence Hills, associated with far-traveled sediment. It is also observed the influence of distinct processes of entrainment sediment on its granulometric and morphoscopic characteristics.