| Latitude : | 69.47948 | |
| Longitude : | -134.58332 | |
| Altitude (m) : | ||
| Startup date : | January 1, 1900 |
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Illisarvik is the site of a long-term experiment in permafrost growth and conditions in and around a drained lake (Mackay 1997; Mackay and Burn 2002). The three primary soil environments in Illisarvik and the surrounding terrain are the drained lake basin
Subsite: MRPILLA / Surficial geology: Ice-rich, high-centre peat polygons with degrading ice wedges under pools of standing water. Peat is more than 300 cm thick. / Vegetation: Peat polygon tundra dominated by evergreen shrubs and low birch. Subsite: MRPILLB / Surficial geology: Till with earth hummocks. / Vegetation: Low shrub tundra dominated by evergreen shrubs, low birch and willow, and sedges. |