Wind-worn rocks (such as "Rillenstein") mostly originate in deserts. But such rocks occur, although less frequently, also in the Netherlands. At first chemical action plays its role, mayor agent is blasting by sandloaded winds.
| Additional Metadata | |
|---|---|
| , , | |
| Grondboor & Hamer | |
| CC BY 3.0 NL ("Naamsvermelding") | |
| Organisation | Nederlandse Geologische Vereniging |
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L.H. Hofland. (1966). Rillensteen. Grondboor & Hamer, 20(5), 216–223. |
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