How to create a "Giant Causeway" landscape with Geomorph

Using the "lift edges" tool and a "water map"

The terraces how-to shows that the "lift edges" tool can be used to create irrigated terraces by superimposing a "water field" with a height field transformed in terraces.

The technique can also be used to improve the realism of a "Giant Causeway"-style rocky seashore, by wetting the top of the basalt pillars.

The scene giant_causeway.pov is provided for this tutorial. It is a derivative of terraces.pov, using different rock texture, terrain scaling and ligthing.




Step 1
- Start with the standard "Subdivision 2" terrain . The example shown was done with a 1024x1024 map. A large height field gives more natural cells boundaries and more latitude to erode the edges of the basalt pillars.

Step 1 - The standard "Subdivision 2" terrain

 

Step 2 - The original terrain almost fills up the full altitude range (0-65535). We need some room to raise the edges of the higher pillars. Choose the "Brightness / Contrast" tool , decrease the contrast by -30 or the like.

Step 3 - Stratify the terrain with the "Giant Causeway" tool . Here a radius of 30 was used, with a line width of 2 and a smoothing radius of 2. Be sure to use a smoothing radius less or equal than the line width, otherwise the "Lift edges" tool would not be able to use the lines between the cells as a "black threshold" - some edges won't be raised.

Step 4 - (Optional) If you want irregular puddles, in the "Giant Causeway" dialog, before accepting the stratification of the terrain, go into the merge subdialog and mix the source and the result at approximately 70% of the result (the default being 100% of the result). This will add some noise on top the the pillars.

Step 4 - To avoid too regular puddles like in this picture,
mix source and result in the Giant Causeway tool




Step 5 - Creation of the water map: If you skipped step 4, clone the terrain with the clone button ("Copy under a new name") in the menu bar , call the clone hf_water.png. If you did step 4, your current map cannot be used as a water map because the top of the pillars are not flat anymore. Then, save your current map under the name you like, create a water map by repeating steps 1 to 3 and save the result as hf_water.png.

Step 6 - Use the "Lift edges" tool on the main terrain. Use the default radius of 20. Unlike the terraces tutorial, you should check the "black threshold" box, to use the lines as edges boundaries. A raising level scale appears after executing the transformation. Try a raising level between 5 and 10. In the current example, a level of 7 was used.

Step 7 - (Optional) If you want slightly irregular edges like in the example shown, use the "Rain erosion" tool on the main terrain, at its defaults settings.

Step 8 - (Optional) If you performed step 7, some water map edges could be too wide and "stick out". Use the "Crests" tool on hf_water.png to narrow the water cells. The default of 3 steps is probably too much, one step would be sufficient.

A section of the main height field, after the edges have been raised and eroded



Step 9 - Choose the default camera 2, render  with giant_causeway.pov.

Step 10 - Fine-tune the contrast with the brightness / constrast tool , if required: Some pillars may appear higher than the water, others lower. If the higher pillars are under the water and the lower pillars over it, increase the terrain contrast. If the higher pillars are over the water and the lower under it, decrease the contrast. A level change of ±1 to ±5 should be sufficient. You can render the scene with different levels before accepting the change. Sometimes you may also have to slightly adjust the brightness.

Here the contrast of the terrain should be tuned to lower the water on higher pillars



Step 11 - In the present case, to fill up the rendered image with the terrain, I edited the giant_causeway.pov file to stretch the terrain in the X and Z directions by a factor of 1.7, and decrease the height by a factor of 0.7. These changes appear as comments in the file distributed with version 0.4. Do not forget to change the scaling of both the terrain and the water map. As usual, the relevant lines in giant_causeway.pov appear after the /**********/ line:

/*******************************************************************************************/

object {hf scale <1,1,1> translate y*0 texture {rock3 scale 0.6}}
// object {hf scale <1.7,0.7,1.7> translate y*0 texture {rock3 scale 0.6}}

#ifdef (water)
    object {water scale <1,1,1>}
//    object {water scale <1.7,0.7,1.7>}
#end

If you feel happy with the vertical scaling (I mean, scale X = scale Y = scale Z), indeed, you don't need to stretch the terrain to fill up the image. Decreasing the camera angle in the preview area is sufficient.

Step 12 - (Optional) The example shown was rotated by 45 degrees with the rotate tool , to get a less straight result. Do not forget to rotate both the main terrain and the water map.

Now the scene can (almost) be used as a building block for a seashore landscape.

Further improvements

There are obviously a few things to improve:

(1) Actual basalt pillars are slighly less regular. One way to simulate this would be to start from the "crack network" tool and fill "regular - perturbated" cells with a stratification of the height field. It is not possible with version 0.40 of Geomorph. Some work for a future version, maybe.

(2) Actual basalt pillars are more crackled, on the X-Z plane and on the Y axis. With version 0.40 of Geomorph, cracks can only be created for the whole map. In real life, X-Z cracks are often bounded by the cells. Vertical cracks (Y) can probably be simulated by a texture applied where the slope is at 90 degrees.

(3) The rock around the puddles does not look wet enough. It is not too difficult to render wet rocks when the water is a plane (see granite reef in the cracks tutorial). But here, puddles are at different levels.  One solution would be to use a wet texture for the whole rock formation to simulate a rainy day... More seriously, it can maybe be solved by a texture map, generated by intersecting the main height field and a water map slightly brighter (higher) than the original one. All the points under the modified water map would have a wet texture. Another solution would be to experiment with a slope texture: the wet parts are generally those where the slope is lower.

Any feedback or suggestion is welcome.
____________________

Written in December 2006

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Contact:    Patrice St-Gelais

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