FondoRichard Moskal Fonds
Serie2023.62 - Ellef Ringnes Island Expedition
Unidad documental compuesta2023.62 - Slide Images
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Unidad documental simple2023.62.142 - Impact of a small stream as it enters the sea waters and ice. Sea ice is melting and broken into bits, but will start freezing quickly in a month or sooner.
Unidad documental simple2023.62.143 - Soil erosion is constant and very natural on the Island. Huge ice lenses below the ground melt quickly and the fine sandy and gravelly wet soils slump away by the forces of gravity.
Unidad documental simple2023.62.144 - Example of how large land areas are being naturally eroded and soils eventually moved to the sea. Interior of Ellef Ringnes Island.
Unidad documental simple2023.62.145 - A very large river delta of water and eroded soil materials entering the sea. Tue sea ice at this location is permanent, except along the shore. Blue water on ice are surface melt water ponds and not open water.
Unidad documental simple2023.62.146 - A very large river delta of water and eroded soil materials entering the sea. Tue sea ice at this location is permanent, except along the shore. Blue water on ice are surface melt water ponds and not open water.
Unidad documental simple2023.62.147 - Close up view of tundra soil erosion and gravity movement. Permafrost ice, when melted made excellent tea or coffee.
Unidad documental simple2023.62.148 - An example of tundra topography, with a meadow of Arctic poppies.
Unidad documental simple2023.62.149 - An example of tundra topography, with a meadow of Arctic poppies.
Unidad documental simple2023.62.150 - An example of tundra topography, with a meadow of Arctic poppies.
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A very large river delta of water and eroded soil materials entering the sea. Tue sea ice at this location is permanent, except along the shore. Blue water on ice are surface melt water ponds and not open water.