6.2.1.2 Hemisphere map

Next: 6.2.2 Stereographic Equal-Angle Projection Up: 6.2.1 Lambert Azimuthal Equal-Area Previous: 6.2.1.1 Rectangular map Contents Index

6.2.1.2 Hemisphere map

Here, you must specify the world as your region (-R0/360/-90/90). E. g., to obtain a hemisphere view that shows the Americas, try

pscoast -Rg -JA280/30/3.5i -B30g30/15g15 -Dc -A1000 -Gblack -P > GMT_lambert_az_hemi.ps

**Figure 6.5:** Hemisphere map using the Lambert azimuthal equal-area projection.
$\begin{figure}\centering\epsfig{figure=eps/GMT_lambert_az_hemi.eps}\end{figure}$

To geologists, the Lambert azimuthal equal-area projection (with origin at 0 $^{o}$ /0 $^{o}$ ) is known as the equal-area (Schmidt) stereonet and used for plotting fold axes, fault planes, and the like. An equal-angle (Wulff) stereonet can be obtained by using the stereographic projection (discussed later). The stereonets produced by these two projections appear below.

**Figure 6.6:** Equal-Area (Schmidt) and Equal-Angle (Wulff) stereo nets.
$\begin{figure}\centering\epsfig{figure=eps/GMT_stereonets.eps}\end{figure}$

Next: 6.2.2 Stereographic Equal-Angle Projection Up: 6.2.1 Lambert Azimuthal Equal-Area Previous: 6.2.1.1 Rectangular map Contents Index

Paul Wessel 2004-10-01