Rocky

Rocky terrain can produce flash floods more easily than you'd expect: thin soils and exposed bedrock reduce infiltration, so intense rain runs off quickly into channels.

Despite "dry-looking" ground, rock can help plants find water-cracks and fractures can funnel and store moisture below the surface, acting like hidden plumbing.

Loose scree slopes can behave like a flowing material: individual rocks creep downhill under freeze-thaw cycles, making the slope slowly "move" over time.

Bare rocks can create their own microclimates-sunny faces heat up dramatically by day, while shaded crevices stay cool and damp, letting very different species live meters apart.

Rocky ground isn't always nutrient-poor: freshly weathered mineral surfaces can release key nutrients, sometimes supporting surprisingly productive patches where fine material accumulates.

High drainage doesn't always mean low moisture for life-dew, fog, and condensation can collect on rock surfaces and drip into cracks, supplying water when rain is scarce.

Rocky terrain can be quieter for roots than it looks: shallow, patchy soils often concentrate roots in small pockets that can be more fertile and stable than surrounding ground.

The "thin soil" problem can sometimes reduce competition: stress-tolerant plants on rocky sites may face fewer fast-growing rivals, giving them an unexpected advantage.

Rocks can protect against temperature extremes: beneath a boulder or within talus, temperatures fluctuate less than in open air, providing refuges for insects, reptiles, and small mammals.

Some rocky slopes have higher infiltration than nearby soils: coarse talus can let water drain rapidly downward into deeper fractures, recharging groundwater rather than staying near the surface.

One of the longest major escarpment systems on Earth is the Great Escarpment of Southern Africa, extending for thousands of kilometers and forming a broad cliff-and-plateau edge around much of the southern African plateau.

Some of the biggest single boulders on Earth are glacial erratics-house-sized rocks transported far from their source and left stranded on rocky ground after ice sheets melted.

Among the most extensive rocky landscapes are stony deserts (regs) and rock pavements, which can cover vast areas and store a long geologic record in their exposed surfaces.

The steepest, most rock-dominated mountain faces host record-setting vertical relief over short distances, where bare bedrock can rise dramatically with little soil development at all.

Some of the longest-lived landforms occur in rocky terrain: ancient bedrock surfaces and tors can persist for millions of years when erosion rates are extremely low.