Inside Antarctica: Ice Sheet, Bedrock, Volcanoes, and Hidden Life
Interior Anatomy
Ice Sheet
- Thickness: up to 4,500 m (15,000 ft) — average 2,160 m.
- Volume: 26.5M km³ (70% Earth’s fresh water).
- Age: Basal ice >1M years; EPICA Dome C core 800 kyr.
- Flow: Gravity-driven — 1–10 m/yr interior, 100–1000 m/yr ice streams.
Bedrock
- East Antarctica: Precambrian shield (granite, gneiss) — stable craton.
- West Antarctica: Rift system, younger sedimentary basins, volcanoes.
- Subglacial lakes: 400+ (Vostok 14,000 km²) — isolated ecosystems.
- Mountains: Gamburtsev (Alps-sized, buried), Transantarctic (exposed).
Volcanoes
- Mt. Erebus (3,794 m) — world’s southernmost active volcano; persistent lava lake.
- Mt. Sidley, Mt. Waesche — dormant.
- Subglacial volcanism influences ice dynamics.
Life
- Coastal: Emperor/Adélie penguins, Weddell/crabeater seals, whales.
- Interior: Nematodes, tardigrades, rotifers, microbes in cryoconite holes.
- Subglacial: Chemosynthetic bacteria (Lake Whillans sampled 2013).
Protection
Antarctic Treaty System (1961) — science only, no mining, military ban. Protocol on Environmental Protection (1998) — strict waste, non-native species, EIA rules.