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[svn r3785] More typos fixed.

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olly 2001-08-15 21:02:01 +02:00
parent b535a13a86
commit e206dea71a
2 changed files with 3 additions and 3 deletions
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2
handbook/survey/ontop.htm
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@ -38,7 +38,7 @@ or get more consistent results by sighting the compass with <b>one</b> eye
rather than two. Remember to do this consistently, and use the same method rather than two. Remember to do this consistently, and use the same method
when doing your calibration. For better accuracy, you should really keep the when doing your calibration. For better accuracy, you should really keep the
survey legs short (6m gives a compass/clino error comparable with a 5cm survey legs short (6m gives a compass/clino error comparable with a 5cm
station postion error). This makes the survey take much longer, and maybe station position error). This makes the survey take much longer, and maybe
more prone to recording errors, so a good compromise is to keep legs down to more prone to recording errors, so a good compromise is to keep legs down to
15m or less, which also makes sketching a little easier. 15m or less, which also makes sketching a little easier.

4
years/1987/geolog.htm
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@ -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 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, 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 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 time, parts of the Calcareous Alpine facies became detached and slid over
others. The main northwards movement leaving the Calcareous Alps in their others. The main northwards movement leaving the Calcareous Alps in their
present position occurred during the Eocene. present position occurred during the Eocene.
@ -68,7 +68,7 @@ depositional environments (facies) can be inferred from the rocks (Fig. 2)
<ol> <ol>
<li>Haupt Dolomit facies. This rock type was laid down behind the main reef, <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 periods of aerial exposure. The facies is mostly characteristic of the
northern part of the Kalkalpen. It interfingers to the south with the northern part of the Kalkalpen. It interfingers to the south with the
Dachstein Limestone (Dachsteinkalk) unit. The maximum thickness of the Haupt Dachstein Limestone (Dachsteinkalk) unit. The maximum thickness of the Haupt