diff --git a/docs/src/man/Blankenbach.md b/docs/src/man/Blankenbach.md
index 10a7f763..ac685201 100644
--- a/docs/src/man/Blankenbach.md
+++ b/docs/src/man/Blankenbach.md
@@ -392,7 +392,11 @@ fig
 
 ### Final model
 Temperature field
-![Temperature](../assets/Blankenbach_Temp.png)
+<!-- ![Temperature](../assets/Blankenbach_Temp.png) -->
+
+<img src="../assets/Blankenbach_Temp.png" width="500"  />
 
 And time history of the rms-velocity and Nusselt number
-![time series](../assets/Blankenbach_Time_Series_V_Nu.png)
+
+<img src="../assets/Blankenbach_Time_Series_V_Nu.png" width="500"  />
+<!-- ![time series](../assets/Blankenbach_Time_Series_V_Nu.png) -->
diff --git a/docs/src/man/ShearBands.md b/docs/src/man/ShearBands.md
index c90591c6..697a0c19 100644
--- a/docs/src/man/ShearBands.md
+++ b/docs/src/man/ShearBands.md
@@ -231,4 +231,5 @@ fig
 
 ### Final model
 Shear Bands evolution in a 2D visco-elasto-plastic rheology model
-![Shearbands](../assets/movies/DP_nx2058_2D.gif)
+
+<img src="../assets/movies/DP_nx2058_2D.gif" width="500"  />
diff --git a/docs/src/man/subduction2D/setup.md b/docs/src/man/subduction2D/setup.md
index a88feba2..3606ded1 100644
--- a/docs/src/man/subduction2D/setup.md
+++ b/docs/src/man/subduction2D/setup.md
@@ -38,7 +38,8 @@ add_box!(
     T       = HalfspaceCoolingTemp(Tsurface=20, Tmantle=Tbot, Age=80,Adiabat=0.4)
 )
 ```
-![](../../assets/Subduction2D_setup_4.png)
+<img src="../../assets/Subduction2D_setup_1.png" width="750"  />
+
 
 Next we add a horizontal 80 km thick oceanic lithosphere. Note that we leave a 100 km buffer zone next to the vertical boundaries of the domain, to facilitate the sliding of the oceanic plates.
 ```julia
@@ -52,7 +53,7 @@ add_box!(
     T       = HalfspaceCoolingTemp(Tsurface=20, Tmantle=Tbot, Age=80, Adiabat=0.4)
 )
 ```
-![](../../assets/Subduction2D_setup_2.png)
+<img src="../../assets/Subduction2D_setup_2.png" width="750"  />
 
 As in the original paper, we add a 8km thick crust on top of the subducting oceanic plate.
 ```julia
@@ -68,9 +69,9 @@ add_box!(
     T       = HalfspaceCoolingTemp(Tsurface=20, Tmantle=Tbot, Age=80, Adiabat=0.4)
 )
 ```
-![](../../assets/Subduction2D_setup_3.png)
+<img src="../../assets/Subduction2D_setup_3.png" width="750"  />
 
-And finally we add the subducting slab, with the trench located at 1430km from the right-hand-side boundary.
+And we add the subducting slab, with the trench located at 1430km from the right-hand-side boundary.
 
 ```julia
 add_box!(
@@ -84,18 +85,12 @@ add_box!(
     T       = HalfspaceCoolingTemp(Tsurface=20, Tmantle=Tbot, Age=80, Adiabat=0.4)
 )
 ```
-![](../../assets/Subduction2D_setup_4.png)
+<img src="../../assets/Subduction2D_setup_4.png" width="750"  />
 
+To finish, we set every cell above the surface to be sticky air, with a temperature of 20°C.
 ```julia
 surf                 = Grid2D.z.val .> 0.0
-@views Temp[surf]   .= 20.0
 @views Phases[surf] .= 3
+@views Temp[surf]   .= 20.0
 ```
-![](../../assets/Subduction2D_setup_5.png)
-
-```julia
-li     = (abs(last(x)-first(x)), abs(last(z)-first(z))) .* 1e3 # in meters
-origin = (x[1], z[1]) .* 1e3 # lower-left corner of the domain
-Phases = Phases[:,1,:] .+ 1  # +1 because Julia is 1-indexed
-Temp   = Temp[:,1,:].+273    # in Kelvin
-```
+<img src="../../assets/Subduction2D_setup_5.png" width="750"  />