Genesis of active sand‐filled polygons in lower and central Beacon Valley, Antarctica

• Published in: Permafrost and Periglacial Processes
• Main Authors: James G. Bockheim, Mark D. Kurz, S. Adam Soule, Andrea Burke
• Format: Article in Journal/Newspaper
• Language: unknown
• Subjects: Breaker; Beacon Valley; Antarc*; Antarctica; Ice; permafrost; wedge*
• Online Access: https://doi.org/10.1002/ppp.661

Nonsorted polygons with sand‐filled wedges were investigated in Beacon Valley, Antarctica (77.82°S, 160.67°E) using field observations coupled with 2‐m resolution aerial photography. A gasoline‐powered concrete breaker was employed to expose the sediments of four polygon centres and six wedges from geomorphic surfaces containing tills of two different ages. The excavated polygons ranged from 9 to 16 m in diameter; the sand‐filled wedges ranged from 0.2 to 2.5 m in width. The top of ice‐bonded permafrost ranged from 12 to 62 cm in depth in the polygon centres and from 64 to >90 cm in wedges. One active thermal‐contraction fissure generally was apparent at the surface, but excavations revealed numerous inactive fissures. The wedges contain sand laminations averaging 3 mm in width when viewed in cross‐section. Although most of the polygons were of the sand‐wedge type, some contained ice veins up to 1 cm in width and could be classed as composite wedges. Three stages of polygon development were observed, including well‐developed polygons on Taylor II surfaces (ca. 117 ka), moderately developed polygons on Taylor III surfaces (ca. 200 ka) and poorly expressed polygons on Taylor IVa and older (ca. >1.1 Ma) surfaces. This retrogressive development may be due to sublimation of ice‐bonded permafrost following thermal cracking. With the drop in ice content, the thermal coefficient of expansion of the permafrost may be lowered, which would result in a reduction in tensile stresses. Copyright © 2009 John Wiley & Sons, Ltd.