Fig. 6
From: Holocene reconfiguration and readvance of the East Antarctic Ice Sheet
JOIDES Trough geometry through which grounding line advance occurs. Initial retreat stabilisation and grounding line advance through GZW progradation appears an unlikely explanation, since the retreated stable position would occur where bed slope (in blue) increases and where trough width (in green) widens. An additional dynamic component is therefore required to drive a readvance
