Total estimated volume of glacier ice located in a river basin. A glacier is defined as the "mass of land ice flowing down a slope (by deformation of its internal structure and by sliding at its base) and enclosed by topographic elements (such as the slopes of a valley or adjacent peaks) surrounding it. The topography of the bedrock is the most influential factor in the dynamics of a glacier and in the slope of its surface. A glacier subsists because of the massive accumulation of snow, which is compensated by the melting of ice at low altitudes or discharge into the sea".
Subdepartment of Environment and Business Statistics - National Statistics Institute
Directorate-General of Water (DGA)
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Hydrometric Network
Annual
Administrative record
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Subdepartment of Environment and Business Statistics - National Statistics Institute
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Annual
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Cubic kilometers (km3)
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Total estimated volume of glacier ice located in a river basin. A glacier is defined as the "mass of land ice flowing down a slope (by deformation of its internal structure and by sliding at its base) and enclosed by topographic elements (such as the slopes of a valley or adjacent peaks) surrounding it. The topography of the bedrock is the most influential factor in the dynamics of a glacier and in the slope of its surface. A glacier subsists because of the massive accumulation of snow, which is compensated by the melting of ice at low altitudes or discharge into the sea".
Subdepartment of Environment and Business Statistics - National Statistics Institute
Administrative record
Directorate-General of Water (DGA)
Hydrometric Network
Annual
-
Cubic kilometers (km3)
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-
-
Annual
-
-
-
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Subdepartment of Environment and Business Statistics - National Statistics Institute
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