@@ -228,9 +228,9 @@ <h2>Geodesic calculations for an ellipsoid done right</h2>
228228 < p >
229229 This page illustrates the geodesic routines available in
230230 JavaScript package
231- < a href ="https://www.npmjs.com/package/geographiclib ">
232- geographiclib, the geodesic routines in GeographicLib </ a >
233- (< a href ="../JavaScript/doc/index.html "> documentation</ a > ).
231+ < a href ="https://www.npmjs.com/package/geographiclib-geodesic ">
232+ geographiclib- geodesic</ a >
233+ (< a href ="../JavaScript/doc/index.html "> documentation</ a > ).
234234 The algorithms are considerably more accurate than Vincenty's
235235 method, and offer more functionality (an inverse method which
236236 never fails to converge, differential properties of the geodesic,
@@ -285,8 +285,8 @@ <h3><a class="anchor" id="inverse">Inverse problem</h3>
285285 Find the shortest path between two points on the earth. The
286286 path is characterized by its length < i > s12</ i > and its azimuth
287287 at the two ends < i > azi1</ i > and < i > azi2</ i > . See
288- < a href ="https://geographiclib.sourceforge.io/html/GeodSolve.1 .html ">
289- GeodSolve(1) </ a >
288+ < a href ="../JavaScript/doc/tutorial-1-geodesics .html ">
289+ this tutorial </ a >
290290 for the definition of the
291291 quantities < i > a12</ i > , < i > m12</ i > , < i > M12</ i > , < i > M21</ i > ,
292292 and < i > S12</ i > . The sample calculation finds the shortest path
@@ -374,8 +374,8 @@ <h3><a class="anchor" id="direct">Direct problem</h3>
374374 with a given azimuth at the starting point. The destination is
375375 characterized by its position < i > lat2, lon2</ i > and its azimuth
376376 at the destination < i > azi2</ i > . See
377- < a href ="https://geographiclib.sourceforge.io/html/GeodSolve.1 .html ">
378- GeodSolve(1) </ a >
377+ < a href ="../JavaScript/doc/tutorial-1-geodesics .html ">
378+ this tutorial </ a >
379379 for the definition of the
380380 quantities < i > a12</ i > , < i > m12</ i > , < i > M12</ i > , < i > M21</ i > ,
381381 and < i > S12</ i > . The sample calculation shows the result of
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