Platzkegel - Versionsgeschichte

Detlev am 17. Mai 2022 um 09:16 Uhr

2022-05-17T09:16:22Z

Detlev: /* Besonderheiten des Platzkegels */

2019-03-30T16:28:33Z

‎Besonderheiten des Platzkegels

Detlev: /* Besonderheiten des Platzkegels */

2019-03-29T13:44:25Z

‎Besonderheiten des Platzkegels

Detlev: /* Besonderheiten des Platzkegels */

2019-03-29T13:43:57Z

‎Besonderheiten des Platzkegels

Detlev: /* Besonderheiten des Platzkegels */

2019-03-29T13:42:27Z

‎Besonderheiten des Platzkegels

Detlev: /* Besonderheiten des Platzkegels */

2019-03-29T13:41:05Z

‎Besonderheiten des Platzkegels

Detlev: /* Lage und Name des Platzkegels */

2019-03-29T13:36:42Z

‎Lage und Name des Platzkegels

Detlev: /* Artikel bearbeitet von : */

2018-12-07T22:02:17Z

‎Artikel bearbeitet von :

Detlev am 7. Dezember 2018 um 22:01 Uhr

2018-12-07T22:01:54Z

Detlev am 7. Dezember 2018 um 22:01 Uhr

2018-12-07T22:01:39Z

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 {{Infobox-Punkt
 |Überschrift = Der Platzkegel}}
 <center>
-<slippymap lat="-3.048811" lon="37.228889" z="11" w="294" h="294" format="jpeg" layer="mapnik" marker="1"/>
+<center><div style="overflow:hidden; border:1px solid #cccccc; margin-bottom:3px; background-color:#f9f9f9; width:294px;">
-</center>
+{{#multimaps: -3.048811, 37.228889 | service = Leaflet | height = 294px | zoom = 11}}
 {{Infobox-Punkt-Bottom
 |Mapunterschrift = Mount Kilimanjaro : Lages des Platzkegels in OprnStreetMap

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 * Und auch in Afrika ist man sich wieder der historischen Namensgebung bewusst.
 <br>Gelesen bei allafrica.com - 14.07.2018 <ref>[https://allafrica.com/stories/201806140546.html allafrica.com] - Tanzania: Unique Snow Attracts On Mt Kilimanjaro, 14.07.2018</ref><div id='zitat'>Noteworthy is its eruptive activity at the Shira Centre that started up about 2.5 million years ago, as well as its last phase that occurred about 1.9 million years ago, just before the northern part of the edifice collapsed.<br>Shira is crowned by a broad plateau at 3,800 metres that may be filled with a caldera, whose caldera rim remnant has been degraded deeply by erosion.<br>Shira is mostly composed of basic lavas with some pyroclastics whose caldera formation was accompanied by lava emanating from ring fractures, but there was no large scale explosive activity.<br>Two cones formed subsequently, the phonolitic one at the northwest end of the ridge and the doleritic <b>"Platzkegel"</b> in the caldera centre.
-<div><br>
+</div><br>
 == Galerie Platzkegel ==

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 * In aktuellen wissenschaftlichen Publikationen wird die Bezeichnung "[[Platzkegel]]" jedoch wieder verwendet. <ref name="halarchives" />
 * Und auch in Afrika ist man sich wieder der historischen Namensgebung bewusst.
-<br>Gelesen bei allafrica.com - 14.07.2018 <ref>[httphttps://allafrica.com/stories/201806140546.html allafrica.com] - Tanzania: Unique Snow Attracts On Mt Kilimanjaro, 14.07.2018</ref><div id='zitat'>Noteworthy is its eruptive activity at the Shira Centre that started up about 2.5 million years ago, as well as its last phase that occurred about 1.9 million years ago, just before the northern part of the edifice collapsed.<br>Shira is crowned by a broad plateau at 3,800 metres that may be filled with a caldera, whose caldera rim remnant has been degraded deeply by erosion.<br>Shira is mostly composed of basic lavas with some pyroclastics whose caldera formation was accompanied by lava emanating from ring fractures, but there was no large scale explosive activity.<br>Two cones formed subsequently, the phonolitic one at the northwest end of the ridge and the doleritic <b>"Platzkegel"</b> in the caldera centre.
+<br>Gelesen bei allafrica.com - 14.07.2018 <ref>[https://allafrica.com/stories/201806140546.html allafrica.com] - Tanzania: Unique Snow Attracts On Mt Kilimanjaro, 14.07.2018</ref><div id='zitat'>Noteworthy is its eruptive activity at the Shira Centre that started up about 2.5 million years ago, as well as its last phase that occurred about 1.9 million years ago, just before the northern part of the edifice collapsed.<br>Shira is crowned by a broad plateau at 3,800 metres that may be filled with a caldera, whose caldera rim remnant has been degraded deeply by erosion.<br>Shira is mostly composed of basic lavas with some pyroclastics whose caldera formation was accompanied by lava emanating from ring fractures, but there was no large scale explosive activity.<br>Two cones formed subsequently, the phonolitic one at the northwest end of the ridge and the doleritic <b>"Platzkegel"</b> in the caldera centre.
 <div><br>

@@ Zeile 30: / Zeile 30: @@
 * In aktuellen wissenschaftlichen Publikationen wird die Bezeichnung "[[Platzkegel]]" jedoch wieder verwendet. <ref name="halarchives" />
 * Und auch in Afrika ist man sich wieder der historischen Namensgebung bewusst.
-<br>Gelesen bei allafrica.com - 14.07.2018 <ref>[httphttps://allafrica.com/stories/201806140546.html allafrica.com] - Tanzania: Unique Snow Attracts On Mt Kilimanjaro, 14.07.2018</ref><div id='zitat'>Noteworthy is its eruptive activity at the Shira Centre that started up about 2.5 million years ago, as well as its last phase that occurred about 1.9 million years ago, just before the northern part of the edifice collapsed.<br>Shira is crowned by a broad plateau at 3,800 metres that may be filled with a caldera, whose caldera rim remnant has been degraded deeply by erosion.<br>Shira is mostly composed of basic lavas with some pyroclastics whose caldera formation was accompanied by lava emanating from ring fractures, but there was no large scale explosive activity.<br>Two cones formed subsequently, the phonolitic one at the northwest end of the ridge and the doleritic "Platzkegel" in the caldera centre.
+<br>Gelesen bei allafrica.com - 14.07.2018 <ref>[httphttps://allafrica.com/stories/201806140546.html allafrica.com] - Tanzania: Unique Snow Attracts On Mt Kilimanjaro, 14.07.2018</ref><div id='zitat'>Noteworthy is its eruptive activity at the Shira Centre that started up about 2.5 million years ago, as well as its last phase that occurred about 1.9 million years ago, just before the northern part of the edifice collapsed.<br>Shira is crowned by a broad plateau at 3,800 metres that may be filled with a caldera, whose caldera rim remnant has been degraded deeply by erosion.<br>Shira is mostly composed of basic lavas with some pyroclastics whose caldera formation was accompanied by lava emanating from ring fractures, but there was no large scale explosive activity.<br>Two cones formed subsequently, the phonolitic one at the northwest end of the ridge and the doleritic <b>"Platzkegel"</b> in the caldera centre.
 <div><br>

@@ Zeile 30: / Zeile 30: @@
 * In aktuellen wissenschaftlichen Publikationen wird die Bezeichnung "[[Platzkegel]]" jedoch wieder verwendet. <ref name="halarchives" />
 * Und auch in Afrika ist man sich wieder der historischen Namensgebung bewusst.
-<br>Gelesen bei allafrica.com <ref>[httphttps://allafrica.com/stories/201806140546.html allafrica.com] - Tanzania: Unique Snow Attracts On Mt Kilimanjaro, 14.07.2018</ref><div id='zitat'>Noteworthy is its eruptive activity at the Shira Centre that started up about 2.5 million years ago, as well as its last phase that occurred about 1.9 million years ago, just before the northern part of the edifice collapsed.
+<br>Gelesen bei allafrica.com - 14.07.2018 <ref>[httphttps://allafrica.com/stories/201806140546.html allafrica.com] - Tanzania: Unique Snow Attracts On Mt Kilimanjaro, 14.07.2018</ref><div id='zitat'>Noteworthy is its eruptive activity at the Shira Centre that started up about 2.5 million years ago, as well as its last phase that occurred about 1.9 million years ago, just before the northern part of the edifice collapsed.<br>Shira is crowned by a broad plateau at 3,800 metres that may be filled with a caldera, whose caldera rim remnant has been degraded deeply by erosion.<br>Shira is mostly composed of basic lavas with some pyroclastics whose caldera formation was accompanied by lava emanating from ring fractures, but there was no large scale explosive activity.<br>Two cones formed subsequently, the phonolitic one at the northwest end of the ridge and the doleritic "Platzkegel" in the caldera centre.
 <div><br>

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 == Lage und Name des Platzkegels ==
 * Der markante, 3.852m hohe Einzelgipfel liegt im Zentrum der [[Shira Kaldera]], die durch die Gipfel der [[Shira Ridge]] umgeben ist. Er besteht aus basaltischen Bruchstücken und Lavaüberzügen.
-* Benannt wurde der Gipfel nach dem Maler [[Ernst Platz]], der das Team um [[Dr. Hans Meyer]] bei der Zweitbesteigung des Kibos im Jahr 1998 begleitete, als "[[Platzkegel]]". <ref name="halarchives">[http://hal.archives-ouvertes.fr/docs/00/30/44/58/PDF/Nonnotte_et_al.J.Volc.Geoth.Res-08.pdf Journal of Volcanology and Geothermal Research], New K-Ar age determinations of Kilimanjaro volcano</ref>
+* Benannt wurde der Gipfel nach dem Maler [[Ernst Platz]], der das Team um [[Dr. Hans Meyer]] bei der Zweitbesteigung des Kibos im Jahr 1898 begleitete, als "[[Platzkegel]]". <ref name="halarchives">[http://hal.archives-ouvertes.fr/docs/00/30/44/58/PDF/Nonnotte_et_al.J.Volc.Geoth.Res-08.pdf Journal of Volcanology and Geothermal Research], New K-Ar age determinations of Kilimanjaro volcano</ref>
 == Besonderheiten des Platzkegels ==

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 [[Kategorie:Das Mount Kilimanjaro Wiki]]
 [[Kategorie:Markante Punkte am Kilimanjaro]]
-[[Kategorie:Artikel mit Google-Maps]]
+[[Kategorie:Artikel mit OpenStreetMap]]