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authorKristian Evers <kristianevers@gmail.com>2019-05-06 17:48:45 +0200
committerGitHub <noreply@github.com>2019-05-06 17:48:45 +0200
commit4636df33ed4d2a9bedf19973d58a42858fb816c0 (patch)
tree067848d644902cbba7933306972e2c53320b3249 /docs/source
parenta16cb05010115690ecca8938d95ca544f2ad65c6 (diff)
parentc8c3f0bec38a643a3d7391213b6dbc99363d75e4 (diff)
downloadPROJ-4636df33ed4d2a9bedf19973d58a42858fb816c0.tar.gz
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Merge pull request #1455 from plimkilde/geodesic_typo_fix
Fix typos in geodesic doc
Diffstat (limited to 'docs/source')
-rw-r--r--docs/source/geodesic.rst4
1 files changed, 2 insertions, 2 deletions
diff --git a/docs/source/geodesic.rst b/docs/source/geodesic.rst
index c7753404..11bb5e5c 100644
--- a/docs/source/geodesic.rst
+++ b/docs/source/geodesic.rst
@@ -93,7 +93,7 @@ The routines also calculate several other quantities of interest
On a flat surface, we have :math:`m_{12}=s_{12}`.
* :math:`M_{12}` and :math:`M_{21}` are geodesic scales. If two
geodesics are parallel at point 1 and separated by a small distance
- :\math`dt`, then they are separated by a distance :math:`M_{12}\,dt` at
+ :math:`dt`, then they are separated by a distance :math:`M_{12}\,dt` at
point 2. :math:`M_{21}` is defined similarly (with the geodesics
being parallel to one another at point 2). :math:`M_{12}` and
:math:`M_{21}` are dimensionless quantities. On a flat surface,
@@ -159,7 +159,7 @@ areas is based on :cite:`Danielsen1989`. These improve on the work of
:cite:`Vincenty1975` in the following respects:
* The results are accurate to round-off for terrestrial ellipsoids (the
- error in the distance is less then 15 nanometers, compared to 0.1 mm
+ error in the distance is less than 15 nanometers, compared to 0.1 mm
for Vincenty).
* The solution of the inverse problem is always found. (Vincenty's
method fails to converge for nearly antipodal points.)