accumulative form of snow topography up to 30 m high, occurring on the slope of ice sheets due to th – Russian translation

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accumulative form of snow topography up to 30 m high, occurring on the slope of ice sheets due to the interaction of permanent winds with the mesorelief of the glacier surface

аккумулятивная форма снежного рельефа высотой до 30 м, возникающая на склоне ледниковых щитов при взаимодействии постоянных ветров с мезорельефом ледниковой поверхности

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