diff --git a/exercises/exercise-basic/README.md b/exercises/exercise-basic/README.md
index 316dc4c836b3c36ad99925c9109e66532d54e8f8..307893ce14755d53e65bc007d1a7d34098fb3b2b 100644
--- a/exercises/exercise-basic/README.md
+++ b/exercises/exercise-basic/README.md
@@ -5,7 +5,7 @@
 N$`_2`$ is injected in an aquifer previously saturated with water with an injection rate of 0.0001 kg/(s*m$`^2`$).
 The aquifer is situated 2700 m below sea level and the domain size is 60 m x 40 m. It consists of two layers, a moderately permeable one ($`\Omega_1`$) and a lower permeable one ($`\Omega_2`$).
 
-<img src="https://git.iws.uni-stuttgart.de/dumux-repositories/dumux/raw/master/tutorial/extradoc/exercise1_setup.png" width="1000">
+<img src="https://git.iws.uni-stuttgart.de/dumux-repositories/dumux-course/raw/master/exercises/extradoc/exercise1_setup.png" width="1000">
 
 ## Preparing the exercise
 
@@ -93,6 +93,6 @@ make exercise1_2pni # builds new executable
 
   __Initial conditions:__ The same temperature gradient as in the boundary conditions with an additional lens (with position: 20 < x < 30, 5 < y < 35), which has an initial temperature of 380 K.
 
-<img src="https://git.iws.uni-stuttgart.de/dumux-repositories/dumux/raw/master/tutorial/extradoc/exercise1_nonisothermal.png" width="800">
+<img src="https://git.iws.uni-stuttgart.de/dumux-repositories/dumux-course/raw/master/exercises/extradoc/exercise1_nonisothermal.png" width="800">
 
 The non-isothermal model requires additional parameters like the thermal conductivity of the solid component. They are already implemented and set in `exercise1.input`, you just need to _uncomment_ them.