commit 38d06e72660037428d4d878c757b36ee9e2a0b71
parent 26002cb3d2afe949005288289cb560489e357b79
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date: Wed, 15 Apr 2026 11:21:17 +0200
018-tem-loader: fix typo
Diffstat:
2 files changed, 4 insertions(+), 4 deletions(-)
diff --git a/pages/018-tem-loader.html b/pages/018-tem-loader.html
@@ -5,7 +5,7 @@
<p>If you run into problems installing or using the plugin, please <a href="mailto:andam@geus.dk">get in touch</a>.</p>
<h2 id="motivation">Motivation</h2>
-<p>The Transient Electromagnetic Method (TEM) geophysics method for imaging subsurface electrical properties from the ground surface or airborne instrumentaiton. The method is popular in ground-water surveys, mineral exploration, and other geological applications where differences in electrical resistivity of the subsurface are of interest.</p>
+<p>The Transient Electromagnetic Method (TEM) is used for imaging subsurface electrical properties from the ground surface or with airborne instrumentation. The method is popular in ground-water surveys, mineral exploration, and other geological applications where differences in electrical resistivity of the subsurface are of interest.</p>
<p>The subsurface resistivities are calculated through numerical inversion, where the observed decay of an induced magnetic field is matched against subsurface properties. The inverted resistivity models are the end goal for the geological analysis, and are typically exported from the inversion software as XYZ text files. The files contain one row per sounding, with a stack of resistivity layers and a depth of investigation. Reading these data usually requires specialized commercial software.</p>
diff --git a/pages/018-tem-loader.txt b/pages/018-tem-loader.txt
@@ -7,9 +7,9 @@ in touch.
## Motivation
-The Transient Electromagnetic Method (TEM) geophysics method for
-imaging subsurface electrical properties from the ground surface
-or airborne instrumentaiton. The method is popular in ground-water
+The Transient Electromagnetic Method (TEM) is used for imaging
+subsurface electrical properties from the ground surface or with
+airborne instrumentaiton. The method is popular in ground-water
surveys, mineral exploration, and other geological applications
where differences in electrical resistivity of the subsurface are
of interest.
