Formation of coastal elfin forests in northern California and Oregon, began with a series of marine terraces. A combination of uplift and changes in ocean level formed a system of terraces, resulting in an “ecological staircase”, with each terrace approximately 100,000 years older than the one below it and supporting a distinct association of soils, microbes, plants, and animals. A dune being pushed farther away from the coast by fluctuating sea levels slides over the one before it and solidifies, raising the terraces. Pioneer plant communities colonize the young terrace. The succession of plant communities that repeats on each terrace eventually forms a very specific podzol known as the Blacklock series, which offers an inhospitable environment for species and greatly stunts further growth on the terrace. Part of this soil profile includes an underlying clay or iron hardpan. Each terrace is relatively level and many are footed by paleo-dunes. Drainage is poor at best on these stairs and plants sit in a bath of their own tannins and acids for much of the wet season. Due to limited root mobility and acidic soil, plant communities on these terraces grow into stunted forms. Remnants of ecological staircases doubtless exist, however most have been destroyed for development or logging.