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<urlset xmlns="http://www.sitemaps.org/schemas/sitemap/0.9" xmlns:image="http://www.google.com/schemas/sitemap-image/1.1"><url><loc>https://saltstraumen-museum.no/Velkommen/?Article=251</loc><lastmod>2026-01-20T09:26:13+01:00</lastmod><image:image><image:loc>https://saltstraumen-museum.no/sites/s/saltstraumen-museum.no/files/2024/04/norsk-fiskevaersmuseum-a-i-lofoten-foto-kjell-ove-storvik-7646.jpg?thumbnail=1000x1000</image:loc></image:image></url><url><loc>https://saltstraumen-museum.no/Velkommen/?Article=251</loc><lastmod>2026-01-20T09:26:13+01:00</lastmod><image:image><image:loc>https://saltstraumen-museum.no/sites/s/saltstraumen-museum.no/files/2024/04/norsk-fiskevaersmuseum-a-i-lofoten-foto-kjell-ove-storvik-7646.jpg?thumbnail=1000x1000</image:loc></image:image></url><url><loc>https://saltstraumen-museum.no/?id=246494733&amp;Article=51</loc><lastmod>2018-10-24T22:20:02+02:00</lastmod><image:image><image:loc>https://saltstraumen-museum.no/sites/s/saltstraumen-museum.no/files/geobro_front.jpg?thumbnail=1000x1000</image:loc></image:image><image:image><image:loc>https://saltstraumen-museum.no/sites/s/saltstraumen-museum.no/files/geobro_fig1.jpg</image:loc><image:caption>Figure 1. The red frame shows the area by the &#xC5;seli Stream described in the text (map detail taken </image:caption></image:image><image:image><image:loc>https://saltstraumen-museum.no/sites/s/saltstraumen-museum.no/files/geobro_fig2.jpg</image:loc><image:caption>Figure 2. An illustration of the collision between Greenland and Norway, the Caledonian mountain fol</image:caption></image:image><image:image><image:loc>https://saltstraumen-museum.no/sites/s/saltstraumen-museum.no/files/geobro_bilde1.jpg</image:loc><image:caption>Photo 1. The Caledonian folded mountains in miniature (photo: Rikke Lunell)</image:caption></image:image><image:image><image:loc>https://saltstraumen-museum.no/sites/s/saltstraumen-museum.no/files/geobro_bilde2.jpg</image:loc><image:caption>Photo 2. Inclined shale with a white dike. The Caledonian folded mountains, originally made from hor</image:caption></image:image><image:image><image:loc>https://saltstraumen-museum.no/sites/s/saltstraumen-museum.no/files/geobro_bilde3.jpg</image:loc><image:caption>Photo 3. The terminal moraine at the &#xC5;seli Stream with larger stones and boulders on top (photo: Ar</image:caption></image:image><image:image><image:loc>https://saltstraumen-museum.no/sites/s/saltstraumen-museum.no/files/geobro_bilde4.jpg</image:loc><image:caption>Photo 4. Strations on Straumsneset at &#xC5;seli. Whether the glacier has moved toward us or away from u</image:caption></image:image><image:image><image:loc>https://saltstraumen-museum.no/sites/s/saltstraumen-museum.no/files/geobro_bilde5.jpg</image:loc><image:caption>Photo 5. The crescentic gouge in this photo show that the glacier at the &#xC5;seli Stream has moved tow</image:caption></image:image><image:image><image:loc>https://saltstraumen-museum.no/sites/s/saltstraumen-museum.no/files/geobro_fig3.jpg</image:loc><image:caption>Figure 3. The diagram shows the formation of a roche moutonn&#xE9;e, as mentioned in the text (illustrat</image:caption></image:image><image:image><image:loc>https://saltstraumen-museum.no/sites/s/saltstraumen-museum.no/files/geobro_bilde6.jpg</image:loc><image:caption>Photo 6. A roche mounton&#xE9;e (center) with the steep leeward side to the left (northwest). The &#xC5;seli</image:caption></image:image></url></urlset>
