Case study · East Asia
Hong Kong slopes
Hong Kong Island · New Territories
Weathered granite, steep catchments, a city on the toe. Holderness is till at the sea; Hong Kong is saprolite on a slope.

Locator · OpenStreetMap / OpenFreeMap · 22.28°, 114.16°
Hong Kong’s hills are granite and volcanic rock, deeply weathered in a subtropical monsoon. The saprolite is thick; joints open; a rain band turns a slope into a debris flow. The 1972 Sau Mau Ping disaster is the classroom sentence: fill and weathered granite, not a chalk cliff.
Compare Holderness. There the budget is waves versus till. Here the budget is rain versus a weathered slope above a dense city. Same syllabus word — mass movement — different rock, different trigger, different map.
The weathering lab’s granite close-up is the mineral story. The mass-movement lab is the failure. A groyne will not save a Hong Kong slope. A cut-and-fill wall might, if the drainage is honest.
Classroom move: open mass-movement, freeze a rotational slide, then jump to the Holderness case. Ask which one the sea wrote and which one the rain wrote before you show the map.
Exam-style question
Contrast a Hong Kong hillslope failure with Holderness cliff retreat, using rock type and the triggering process.
Teacher hint: Hong Kong: weathered granite + intense rain. Holderness: glacial till + waves. Same word (mass movement / erosion), different agents.
Process labs
Sources
- GEO Hong Kong — landslide studies
- BGS — Holderness till