hat
Tli Santral Lowlands se yon fon Rift sitou comprenant fòmasyon paleyozoyik yo. Anpil nan sediman sa yo gen siyifikasyon ekonomik pou li se isit la ke chabon ak fè pitit fè wòch yo ki alimenté revolisyon endistriyèl Scotland a yo dwe jwenn. Zòn sa a te tou ki gen eksperyans entans volkanism, Syèj Arthur a nan Edinburgh ke yo te ti rès ki rete nan yon vòlkan yon fwa pi gwo. Zòn sa a se relativman ki nan altitid ba, byenke menm isit la ti mòn tankou Ochils yo ak Campsie FELLS yo se raman lwen soti nan vi.
eng
The Central Lowlands is a rift valley mainly comprising Paleozoic formations. Many of these sediments have economic significance for it is here that the coal and iron bearing rocks that fuelled Scotland's industrial revolution are to be found. This area has also experienced intense volcanism, Arthur’s Seat in Edinburgh being the remnant of a once much larger volcano. This area is relatively low-lying, although even here hills such as the Ochils and Campsie Fells are rarely far from view.