[svn r3785] More typos fixed.

years/1987/geolog.htm

@@ -55,7 +55,7 @@ the photic zone, resulting in deep water sediments rather than reefs. It can
 be concluded that subsidence was more rapid in the south of the depositional
 area during the Triassic. In the Jurassic, the pattern of subsidence changed,
 affecting the facies belts. There may have been local areas of elevation. In
-some areas depostion continued into the Cretaceous. During Late Cretaceous
+some areas deposition continued into the Cretaceous. During Late Cretaceous
 time, parts of the Calcareous Alpine facies became detached and slid over
 others. The main northwards movement leaving the Calcareous Alps in their
 present position occurred during the Eocene.
@@ -68,7 +68,7 @@ depositional environments (facies) can be inferred from the rocks (Fig. 2)
 
 <ol>
 <li>Haupt Dolomit facies. This rock type was laid down behind the main reef,
-in the quiet back reef lagoon. Cycles of depostion are apparent as are
+in the quiet back reef lagoon. Cycles of deposition are apparent as are
 periods of aerial exposure. The facies is mostly characteristic of the
 northern part of the Kalkalpen. It interfingers to the south with the
 Dachstein Limestone (Dachsteinkalk) unit. The maximum thickness of the Haupt