The conclusions of the project were that: (a) some glaciers, including Upsala, Onelli, Bolados, Frías and Dickson, whose front sides were based on lakes, had seen their glacier tongues recede in the last two decades; (b) several slope glaciers, including Murallón, had shown serious degradation; (c) several glaciers with areas smaller than 2 square km had practically disappeared; (d) some glaciers, including Viedma, had become significantly smaller, especially in ablation areas; (e) there were very clearly defined moraines in valleys between glaciers, indicating further disintegration in the higher parts of mountain ranges due to erosion from exogenous agents; (f) glaciers at the same latitude were undergoing very different changes.