diff --git a/cave_data/1623-2023-mg-03.html b/cave_data/1623-2023-mg-03.html
index 169ad0adc..4cb2103c1 100644
--- a/cave_data/1623-2023-mg-03.html
+++ b/cave_data/1623-2023-mg-03.html
@@ -1,5 +1,5 @@
 <!DOCTYPE html>
-<!-- This file is generated by troggle on July 13, 2023, 11:09 p.m. UTC using the form documented at /handbook/survey/caveentry.html -->
+<!-- This file is generated by troggle on July 13, 2023, 11:11 p.m. UTC using the form documented at /handbook/survey/caveentry.html -->
 <!-- Only put one cave in this file -->
 <!-- If you edit this 1623-nnn.html file by hand, and manually upload it to the server using git,
 make sure you update the database by doing a full data import. If you edit it using the online form
@@ -10,7 +10,7 @@ though, you do not need to do a data import as it happens automatically -->
 <meta http-equiv="Content-Type" content="text/html; charset=UTF-8"/>
 </head>
 <body>
-<b>This file is generated by troggle</b> on July 13, 2023, 11:09 p.m. UTC using the form documented at
+<b>This file is generated by troggle</b> on July 13, 2023, 11:11 p.m. UTC using the form documented at
 the form documented at 
 <a href="/handbook/survey/caveentry.html">handbook/survey/caveentry.html</a>
 <br>
@@ -59,7 +59,7 @@ code used in the Austrian kataster e.g '1/S +' - https://expo/.survex.com/katast
 </entrance>
 
 <explorers>Martin Green, Janis Huns, Zac Woodford</explorers><!-- 'CUCC Expo' and year(s) of exploration. To distinguish from caves explored by foreign groups. Individual names can be given too if it was a small cave. -->
-<survex_file>1623.2023-mg-03</survex_file><!-- Name of top-level survey file for this cave. Relative to the 'loser' survex repository. So for most caves that's "caves/cavenum/cavnum.svx". (e.g. caves/204/204.svx -->
+<survex_file>caves-1623.2023-mg-03</survex_file><!-- Name of top-level survey file for this cave. Relative to the 'loser' survex repository. So for most caves that's "caves/cavenum/cavnum.svx". (e.g. caves/204/204.svx -->
 <underground_description><p>Cold Salamander Cave is formed along an obvious surfacee weakness going from SW to NE.  In 2023 the most south westely entrance (A), could be down climbed for 2m to a snow pile.  This was descended with the aid of a handline into a significant chamber.  A few metres to the North East another shaft (B) also entered but with a pitch down to the snow slope.  The chamber is deorated with several 4m long icicles and a stationary Salamander.</p>
 
 <a href='/1623/2023-mg-03/l/pls_make_this_my_mugshot.html'><img src='/1623/2023-mg-03/t/pls_make_this_my_mugshot.jpg' /></a>
