- ArquivoRichard Moskal Fonds
- Série2023.62 - Ellef Ringnes Island Expedition
- Documento2023.62 - Slide Images
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- Item2023.62.140 - Isachsen weather station in summer. The coastal sea ice has melted. Same coast where we did the sea ice black dirt experiments earlier in the summer.
- Item2023.62.141 - Richard Moskal at Isachsen. The beard has grown and I returned to Ottawa with it still intact.
- Item2023.62.142 - 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.
- Item2023.62.143 - 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.
- Item2023.62.144 - Example of how large land areas are being naturally eroded and soils eventually moved to the sea. Interior of Ellef Ringnes Island.
- Item2023.62.145 - 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.
- Item2023.62.146 - 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.
- Item2023.62.147 - Close up view of tundra soil erosion and gravity movement. Permafrost ice, when melted made excellent tea or coffee.
- Item2023.62.148 - An example of tundra topography, with a meadow of Arctic poppies.
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