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fix up URLs in static html for ${subarea} -> '1623' that have no

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Wookey
2015-04-08 03:18:59 +01:00
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years/1977/report.htm
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@@ -81,7 +81,7 @@
<p><img src="106.png" alt="106 survey - 19k gif" width="640" height="860" /></p>
<hr />
<h3><a name="nicknotes">Some Notes</a> on the <span lang="de-at">Loser</span> Plateau</h3>
<p>In the absence, as we are given to understand, of any detailed study of the <span lang="de-at">loser/Sch&ouml;nberg</span> plateau, it is difficult to write with any authority on the hydrology and geology of the area. We were further handicapped by a lack of adequately contoured large-scale maps from which spot heights could be assessed. Still, the following points may be of interest.</p>
<p>In the absence, as we are given to understand, of any detailed study of the <span lang="de-at">1623/Sch&ouml;nberg</span> plateau, it is difficult to write with any authority on the hydrology and geology of the area. We were further handicapped by a lack of adequately contoured large-scale maps from which spot heights could be assessed. Still, the following points may be of interest.</p>
<p>The part of the plateau with which we were concerned takes the rough form of a wide and shallow cirque, bounded to the south by the impervious (dolomitic?) shales of the <span lang="de-at">Br&auml;uning</span> Wall, to the east by the peaks of the <span lang="de-at">Schwarzmooskogel</span> and <span lang="de-at">Augsteck</span>, and to the north by the <span lang="de-at">Sch&ouml;nberg</span>. The slope - and as far as we could judge - the general dip are WSW, and the bulk of the plateau falls within the altitude range 1600-1800m. Several sizeable valleys appear to coalesce in the centre of the plateau, but in the short time available to us we were only able to explore a small area within about 1&nbsp;km from the <span lang="de-at">Schwarzmoos-Sattel</span>. Given the size of the plateau, its patches of dense scrub, and its orogenetic and morphogenetic complexity we can only guess at the character of the parts left unexplored, but we think it very unlikely that there will be any integrated surface flow or stream sinks.</p>
<p><img src="map.png" alt="sketch map of area - 20k gif" width="735" height="940" /></p>
<p><span lang="de-at">Karl Gaisberger</span> informed us that a dye-test in the <span lang="de-at">Augstsee</span> (a small lake near our route up to the plateau) had given a positive trace to the water mains of <span lang="de-at">Bad Ischl</span>, some 12km to the west. Unfortunately, <span lang="de-at">Bad Ischl</span> is fed by several tapped springs and it had not been possible to identify the exact one. We do know though (1) that a spring near or in <span lang="de-at">Naglstegh&ouml;hle</span> has been tested from the <span lang="de-at">Steyrer-See</span> near <span lang="de-at">Tauplitz</span>, a trace distance of about 30km. Since the <span lang="de-at">Loser</span> Plateau lies on this traceline it is a simplistic but fair assumption that the water from our discoveries also resurges there.</p>