Botanical Geology
How Flowers Reveal Bedrock Chemistry
You can often identify bedrock without hitting it with a hammer simply by noting what blooms in the scree. Acidic quartzites and granites in Rondane support sparse, hardy species: Highland Rush, Crowberry, and yellow-green map lichens. Cross onto the calcareous phyllites and greenstones of Knutshøe on Dovrefjell or inner Troms, and the turf erupts with eight-petalled white Mountain Avens (Dryas octopetala), Purple Saxifrage (Saxifraga oppositifolia), and rare alpine gentians.
Snow Cover Gradient
The Ridge-to-Hollow Microclimate
In winter, strong mountain winds sweep snow off convex ridges (rabbe) and pack it meters deep into concave leeward hollows (snøleie). This creates a sharp ecological sequence over a horizontal distance of less than twenty metres:
1. Exposed Ridge Crest: Snow-free all winter. Plants must endure severe frost and dehydrating winds, but they start photosynthesising in May. Only woody prostrate mats like Trailing Azalea and Diapensia survive here.
2. Leeward Heath Slope: Protected by 50–150 cm of insulating winter snow (which keeps ground temperatures near -1°C to -3°C) yet melts out by early June. Ideal for Bilberry, Blue Heath (Phyllodoce caerulea), and Dwarf Birch.
3. Late Snowbed: Buried under snow until late July. Plants here avoid winter frost entirely, but must complete leafing, flowering, and seed set in just five weeks. Look for tiny Dwarf Willow (Salix herbacea) and Starry Saxifrage.