Strathmore (Gaelic: An Srath Mòr) is a strath in east central Scotland running from northeast to southwest between the Grampian mountains and the Sidlaws.It is approximately 50 miles (80 km) long and 10 miles (16 km) wide. Strathmore is underlain by Old Red Sandstone but this is largely obscured by glacial till, sands and gravels deposited during the ice age. Its northeast to southwest alignment is influenced by the underlying geological structure of the area which reflects the dominant Caledonian trend of both the central lowlands and the Highlands of Scotland; its northern margin reflects the presence of the Highland Boundary Fault. Strathmore is fertile and has some of Scotland's best arable farmland, producing soft fruits and cereals.
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| - Strathmore (Gaelic: An Srath Mòr) is a strath in east central Scotland running from northeast to southwest between the Grampian mountains and the Sidlaws.It is approximately 50 miles (80 km) long and 10 miles (16 km) wide. Strathmore is underlain by Old Red Sandstone but this is largely obscured by glacial till, sands and gravels deposited during the ice age. Its northeast to southwest alignment is influenced by the underlying geological structure of the area which reflects the dominant Caledonian trend of both the central lowlands and the Highlands of Scotland; its northern margin reflects the presence of the Highland Boundary Fault. Strathmore is fertile and has some of Scotland's best arable farmland, producing soft fruits and cereals. (en)
- Strathmore (in gaelico scozzese: An Srath Mòr) è uno strath nella Scozia centro-orientale che si estende da nord-est a sud-ovest tra i monti Grampiani e i . È lungo circa 50 miglia (80 km) e largo 10 miglia (16 km). Strathmore è alla base dell'Old Red Sandstone, ma questo è in gran parte oscurato da depositi glaciali, sabbie e ghiaie depositati durante l'era glaciale. Il suo allineamento da nord-est a sud-ovest è influenzato dalla struttura geologica sottostante dell'area che riflette la tendenza Caledoniana dominante sia delle Central Lowlands che delle Highlands scozzesi; il suo margine settentrionale riflette la presenza della faglia di confine delle Highlands. Strathmore è fertile e possiede alcuni dei migliori terreni coltivabili della Scozia, che producono frutti di bosco e cereali. (it)
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| - Strathmore (Gaelic: An Srath Mòr) is a strath in east central Scotland running from northeast to southwest between the Grampian mountains and the Sidlaws.It is approximately 50 miles (80 km) long and 10 miles (16 km) wide. Strathmore is underlain by Old Red Sandstone but this is largely obscured by glacial till, sands and gravels deposited during the ice age. Its northeast to southwest alignment is influenced by the underlying geological structure of the area which reflects the dominant Caledonian trend of both the central lowlands and the Highlands of Scotland; its northern margin reflects the presence of the Highland Boundary Fault. Strathmore is fertile and has some of Scotland's best arable farmland, producing soft fruits and cereals. (en)
- Strathmore (in gaelico scozzese: An Srath Mòr) è uno strath nella Scozia centro-orientale che si estende da nord-est a sud-ovest tra i monti Grampiani e i . È lungo circa 50 miglia (80 km) e largo 10 miglia (16 km). Strathmore è alla base dell'Old Red Sandstone, ma questo è in gran parte oscurato da depositi glaciali, sabbie e ghiaie depositati durante l'era glaciale. Il suo allineamento da nord-est a sud-ovest è influenzato dalla struttura geologica sottostante dell'area che riflette la tendenza Caledoniana dominante sia delle Central Lowlands che delle Highlands scozzesi; il suo margine settentrionale riflette la presenza della faglia di confine delle Highlands. Strathmore è fertile e possiede alcuni dei migliori terreni coltivabili della Scozia, che producono frutti di bosco e cereali. (it)
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