![\"Looking](\"http:\/\/blogs.uml.edu\/antarctica-2015\/wp-content\/uploads\/sites\/36\/2015\/11\/SFmove05.jpg\")
<\/a>Looking across Don Juan Pond onto the viscous flow lobe and our campsite.<\/p><\/div>\n
As you travel east from Don Juan, you go up a fairly gentle slope, encountering several other ponds along the way. One pond was frozen, although Jay tells us that usually it\u2019s salty enough that it remains unfrozen in November. Another pond was almost completely dried up, with only a tiny liquid puddle about a meter across hiding under a boulder.<\/p>\n
<\/a>Frozen pond east of Don Juan.<\/p><\/div>\n
West of Don Juan is the steeper, much more boulder-rich surface of the flow lobe. It\u2019s rough hiking, though not nearly as bad as the treacherously wobbly footing at Sollas Glacier. You\u2019re surrounded by extremely steep cliffs, with bedrock looming vertically above scree slopes. There\u2019s certainly plenty of sediment coming off of the cliffs to keep adding to the flow lobe.<\/p>\n
<\/a>Looking toward the Asgards from South Fork\u2019s main viscous flow lobe.<\/p><\/div>\n
We\u2019ll spend the next two or so weeks here, and then this field season is done!<\/p>\n","protected":false},"excerpt":{"rendered":"
Although Jay has been to South Fork each of his eight seasons in Antarctica, the rest of us needed to get a feel for the valley. We spent Saturday hiking a ways east of Don Juan Pond, and then back … Continue reading