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	<id>https://seligon.conlang.org/index.php?action=history&amp;feed=atom&amp;title=Oshal_Falls</id>
	<title>Oshal Falls - Revision history</title>
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	<updated>2026-04-08T03:46:46Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://seligon.conlang.org/index.php?title=Oshal_Falls&amp;diff=928&amp;oldid=prev</id>
		<title>Michaelmgoessler at 17:04, 27 September 2023</title>
		<link rel="alternate" type="text/html" href="https://seligon.conlang.org/index.php?title=Oshal_Falls&amp;diff=928&amp;oldid=prev"/>
		<updated>2023-09-27T17:04:50Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 17:04, 27 September 2023&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;The &amp;#039;&amp;#039;&amp;#039;Oshal Falls&amp;#039;&amp;#039;&amp;#039; are a major system of waterfalls formed by the [[River Kalpa]] exiting the [[Mountains of Mōrya]] and entering the [[Geranian Heath]].  &lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;The &amp;#039;&amp;#039;&amp;#039;Oshal Falls&amp;#039;&amp;#039;&amp;#039; are a major system of waterfalls formed by the [[River Kalpa]] exiting the [[Mountains of Mōrya]] and entering the [[Geranian Heath]].  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;br/&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;br/&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;=Etymology=&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;=&lt;/ins&gt;=Etymology&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;=&lt;/ins&gt;=&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;The name of the falls harkens back to the term denoting ‘north’ in the [[Old Kattasian language]], &amp;#039;&amp;#039;Oṣṣale&amp;#039;&amp;#039;, either in a (lost) Kattasian name referring to the feature as the ‘northern falls’ or later applied in a designation ‘falls of the Oshale’, after the [[Oshale|region of the same name]].  &lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;The name of the falls harkens back to the term denoting ‘north’ in the [[Old Kattasian language]], &amp;#039;&amp;#039;Oṣṣale&amp;#039;&amp;#039;, either in a (lost) Kattasian name referring to the feature as the ‘northern falls’ or later applied in a designation ‘falls of the Oshale’, after the [[Oshale|region of the same name]].  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;br/&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;br/&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;=Description=&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;=&lt;/ins&gt;=Description&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;=&lt;/ins&gt;=&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;The falls occur at the confluence of the Kalpa, hailing from the [[Mountains of Mōrya#Geography|Mountains of Dôr]], with the [[Yula River]] from [[Uri Téris]]. Entering the [[Geranian Heath]], the conjoining rivers cross the &amp;#039;&amp;#039;&amp;#039;Oshalic Stairs&amp;#039;&amp;#039;&amp;#039;, a series of cliffs and bluffs on the edge of the [[Mountains of Mōrya]] produced in the [[Celdic Thrust Zone]]. Over a stretch of 28 leaps (c. 170m), a varying number of separating and rejoining streams overcome a height difference of a total of 34 leaps (c. 200m), the greatest single drop measuring 18 leaps (c. 100m) on its own. By the time the streams have reached the bottom of the cliff, they have conjoined into one coherent body of water, the [[Kalpa|Kalpa River]].&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;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;&quot;&gt;&lt;div&gt;The falls occur at the confluence of the Kalpa, hailing from the [[Mountains of Mōrya#Geography|Mountains of Dôr]], with the [[Yula River]] from [[Uri Téris]]. Entering the [[Geranian Heath]], the conjoining rivers cross the &amp;#039;&amp;#039;&amp;#039;Oshalic Stairs&amp;#039;&amp;#039;&amp;#039;, a series of cliffs and bluffs on the edge of the [[Mountains of Mōrya]] produced in the [[Celdic Thrust Zone]]. Over a stretch of 28 leaps (c. 170m), a varying number of separating and rejoining streams overcome a height difference of a total of 34 leaps (c. 200m), the greatest single drop measuring 18 leaps (c. 100m) on its own. By the time the streams have reached the bottom of the cliff, they have conjoined into one coherent body of water, the [[Kalpa|Kalpa River]].&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Michaelmgoessler</name></author>
	</entry>
	<entry>
		<id>https://seligon.conlang.org/index.php?title=Oshal_Falls&amp;diff=919&amp;oldid=prev</id>
		<title>Michaelmgoessler: Created page with &quot;The &#039;&#039;&#039;Oshal Falls&#039;&#039;&#039; are a major system of waterfalls formed by the River Kalpa exiting the Mountains of Mōrya and entering the Geranian Heath.   =Etymology= The...&quot;</title>
		<link rel="alternate" type="text/html" href="https://seligon.conlang.org/index.php?title=Oshal_Falls&amp;diff=919&amp;oldid=prev"/>
		<updated>2023-09-27T12:09:08Z</updated>

		<summary type="html">&lt;p&gt;Created page with &amp;quot;The &amp;#039;&amp;#039;&amp;#039;Oshal Falls&amp;#039;&amp;#039;&amp;#039; are a major system of waterfalls formed by the &lt;a href=&quot;/world/River_Kalpa&quot; class=&quot;mw-redirect&quot; title=&quot;River Kalpa&quot;&gt;River Kalpa&lt;/a&gt; exiting the &lt;a href=&quot;/world/Mountains_of_M%C5%8Drya&quot; title=&quot;Mountains of Mōrya&quot;&gt;Mountains of Mōrya&lt;/a&gt; and entering the &lt;a href=&quot;/index.php?title=Geranian_Heath&amp;amp;action=edit&amp;amp;redlink=1&quot; class=&quot;new&quot; title=&quot;Geranian Heath (page does not exist)&quot;&gt;Geranian Heath&lt;/a&gt;.   =Etymology= The...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;The &amp;#039;&amp;#039;&amp;#039;Oshal Falls&amp;#039;&amp;#039;&amp;#039; are a major system of waterfalls formed by the [[River Kalpa]] exiting the [[Mountains of Mōrya]] and entering the [[Geranian Heath]]. &lt;br /&gt;
&lt;br /&gt;
=Etymology=&lt;br /&gt;
The name of the falls harkens back to the term denoting ‘north’ in the [[Old Kattasian language]], &amp;#039;&amp;#039;Oṣṣale&amp;#039;&amp;#039;, either in a (lost) Kattasian name referring to the feature as the ‘northern falls’ or later applied in a designation ‘falls of the Oshale’, after the [[Oshale|region of the same name]]. &lt;br /&gt;
&lt;br /&gt;
=Description=&lt;br /&gt;
The falls occur at the confluence of the Kalpa, hailing from the [[Mountains of Mōrya#Geography|Mountains of Dôr]], with the [[Yula River]] from [[Uri Téris]]. Entering the [[Geranian Heath]], the conjoining rivers cross the &amp;#039;&amp;#039;&amp;#039;Oshalic Stairs&amp;#039;&amp;#039;&amp;#039;, a series of cliffs and bluffs on the edge of the [[Mountains of Mōrya]] produced in the [[Celdic Thrust Zone]]. Over a stretch of 28 leaps (c. 170m), a varying number of separating and rejoining streams overcome a height difference of a total of 34 leaps (c. 200m), the greatest single drop measuring 18 leaps (c. 100m) on its own. By the time the streams have reached the bottom of the cliff, they have conjoined into one coherent body of water, the [[Kalpa|Kalpa River]].&lt;/div&gt;</summary>
		<author><name>Michaelmgoessler</name></author>
	</entry>
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