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Datei:Cariboo Mountains.jpg - Versionsgeschichte
2024-03-28T14:20:05Z
Versionsgeschichte dieser Seite in Klimawandel
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Dieter Kasang: /* Lizenzhinweis */
2020-02-24T13:28:47Z
<p><span dir="auto"><span class="autocomment">Lizenzhinweis</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Version vom 24. Februar 2020, 14:28 Uhr</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Quelle: Beedle, M.J., B. Menounos, and R. Wheate (2015): Glacier change in the Cariboo Mountains, British Columbia, Canada (1952–2005), The Cryosphere, 9, 65–80<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Quelle: Beedle, M.J., B. Menounos, and R. Wheate (2015): Glacier change in the Cariboo Mountains, British Columbia, Canada (1952–2005), The Cryosphere, 9, 65–80<br></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Lizenz: CC BY</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Lizenz: <ins style="font-weight: bold; text-decoration: none;">[https://creativecommons.org/licenses/by/4.0/legalcode.en </ins>CC BY<ins style="font-weight: bold; text-decoration: none;">]</ins></div></td></tr>
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Dieter Kasang
https://wiki.bildungsserver.de/klimawandel/index.php?title=Datei:Cariboo_Mountains.jpg&diff=25303&oldid=prev
Dieter Kasang: /* Lizenzhinweis */
2019-12-02T20:19:17Z
<p><span dir="auto"><span class="autocomment">Lizenzhinweis</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Version vom 2. Dezember 2019, 21:19 Uhr</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Quelle: Beedle, M.J., B. Menounos, and R. Wheate (2015): Glacier change in the Cariboo Mountains, British Columbia, Canada (1952–2005), The Cryosphere, 9, 65–80<<del style="font-weight: bold; text-decoration: none;">/</del>br></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Quelle: Beedle, M.J., B. Menounos, and R. Wheate (2015): Glacier change in the Cariboo Mountains, British Columbia, Canada (1952–2005), The Cryosphere, 9, 65–80<br></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">Zum Copyright der Zeitschrift The Cryospere</del>: <del style="font-weight: bold; text-decoration: none;"> </del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Lizenz</ins>: <ins style="font-weight: bold; text-decoration: none;">CC BY</ins></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">[http://www.the-cryosphere.net/general_information/license_and_copyright.html License and Copyright Agreement]: "The article and any associated published material is distributed under the Creative Commons Attribution 3.0 License"</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
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Dieter Kasang
https://wiki.bildungsserver.de/klimawandel/index.php?title=Datei:Cariboo_Mountains.jpg&diff=19100&oldid=prev
Dieter Kasang: Dieter Kasang lud eine neue Version von „Datei:Cariboo Mountains.jpg“ hoch: Gletschergebiete in den Cariboo Mountains (BC: British Columbia, AB: Alberta)
==Lizenzhinweis==
{| style="border:1px solid #8888aa; background-color:#f7f8ff;padding:5px;fo
2015-04-23T14:03:14Z
<p>Dieter Kasang lud eine neue Version von „<a href="/klimawandel/index.php/Datei:Cariboo_Mountains.jpg" title="Datei:Cariboo Mountains.jpg">Datei:Cariboo Mountains.jpg</a>“ hoch: Gletschergebiete in den Cariboo Mountains (BC: British Columbia, AB: Alberta) ==Lizenzhinweis== {| style="border:1px solid #8888aa; background-color:#f7f8ff;padding:5px;fo</p>
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<td colspan="1" style="background-color: #fff; color: #202122; text-align: center;">Version vom 23. April 2015, 15:03 Uhr</td>
</tr><tr><td colspan="2" class="diff-notice" lang="de-x-formal"><div class="mw-diff-empty">(kein Unterschied)</div>
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Dieter Kasang
https://wiki.bildungsserver.de/klimawandel/index.php?title=Datei:Cariboo_Mountains.jpg&diff=19096&oldid=prev
Dieter Kasang am 22. April 2015 um 13:52 Uhr
2015-04-22T13:52:31Z
<p></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Version vom 22. April 2015, 14:52 Uhr</td>
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<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">Gletscherrückgang auf dem Kilimandscharo. Grün: die eisbedeckten Flächen 1912 nach der Neuberechnung von N.J. Cullen et al. </del>(<del style="font-weight: bold; text-decoration: none;">s. Lizenzhinweis), grau</del>: <del style="font-weight: bold; text-decoration: none;">die eisbedeckten Flächen 2011; Schrift schwarz/kursiv: Namen der wichtigsten Eisfelder</del>, <del style="font-weight: bold; text-decoration: none;">Schrift balu/kursiv</del>: <del style="font-weight: bold; text-decoration: none;">Namen wichtiger Gletscher; Linien blau/gestrichelt: Flächenberechnung 1912 durch Hastenrath, S. and L. Greischar (1997</del>)<del style="font-weight: bold; text-decoration: none;">: Glacier recession on Kilimanjaro, East Africa, 1912–89,</del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Gletschergebiete in den Cariboo Mountains </ins>(<ins style="font-weight: bold; text-decoration: none;">BC</ins>: <ins style="font-weight: bold; text-decoration: none;">British Columbia</ins>, <ins style="font-weight: bold; text-decoration: none;">AB</ins>: <ins style="font-weight: bold; text-decoration: none;">Alberta</ins>)</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">J. Glaciol. 43, 455–459, Linien blau/gestrichelt: Höhenlinien mit m-Angaben</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Lizenzhinweis==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Lizenzhinweis==</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| style="border:1px solid #8888aa; background-color:#f7f8ff;padding:5px;font-size:95%;"</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{| style="border:1px solid #8888aa; background-color:#f7f8ff;padding:5px;font-size:95%;"</div></td></tr>
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Dieter Kasang
https://wiki.bildungsserver.de/klimawandel/index.php?title=Datei:Cariboo_Mountains.jpg&diff=19095&oldid=prev
Dieter Kasang: Gletscherrückgang auf dem Kilimandscharo. Grün: die eisbedeckten Flächen 1912 nach der Neuberechnung von N.J. Cullen et al. (s. Lizenzhinweis), grau: die eisbedeckten Flächen 2011; Schrift schwarz/kursiv: Namen der wichtigsten Eisfelder, Schrift ba…
2015-04-22T13:50:33Z
<p>Gletscherrückgang auf dem Kilimandscharo. Grün: die eisbedeckten Flächen 1912 nach der Neuberechnung von N.J. Cullen et al. (s. Lizenzhinweis), grau: die eisbedeckten Flächen 2011; Schrift schwarz/kursiv: Namen der wichtigsten Eisfelder, Schrift ba…</p>
<p><b>Neue Seite</b></p><div>Gletscherrückgang auf dem Kilimandscharo. Grün: die eisbedeckten Flächen 1912 nach der Neuberechnung von N.J. Cullen et al. (s. Lizenzhinweis), grau: die eisbedeckten Flächen 2011; Schrift schwarz/kursiv: Namen der wichtigsten Eisfelder, Schrift balu/kursiv: Namen wichtiger Gletscher; Linien blau/gestrichelt: Flächenberechnung 1912 durch Hastenrath, S. and L. Greischar (1997): Glacier recession on Kilimanjaro, East Africa, 1912–89,<br />
J. Glaciol. 43, 455–459, Linien blau/gestrichelt: Höhenlinien mit m-Angaben<br />
==Lizenzhinweis==<br />
{| style="border:1px solid #8888aa; background-color:#f7f8ff;padding:5px;font-size:95%;"<br />
|<br />
Quelle: Beedle, M.J., B. Menounos, and R. Wheate (2015): Glacier change in the Cariboo Mountains, British Columbia, Canada (1952–2005), The Cryosphere, 9, 65–80</br><br />
Zum Copyright der Zeitschrift The Cryospere: <br />
[http://www.the-cryosphere.net/general_information/license_and_copyright.html License and Copyright Agreement]: "The article and any associated published material is distributed under the Creative Commons Attribution 3.0 License"<br />
|}</div>
Dieter Kasang