Cuillin range. Cracks and fissures in the rock provided pathways for later magma intrusions, leading to dykes of basalt which are commonly seen across Skye. The Red Cuillin also have volcanic origins, being formed from a later intrusion of acidic, granitic rock. This granite was more uniformly eroded by wind and water than the gabbro and basalt, causing the red hills to have smoother outlines. The Cuillin provide classic examples of glacial topography and were the subject of an early published account by James Forbes in 1846 (who had become a fellow of the Royal Society of Edinburgh aged only nineteen).
On the Hills of Manchuria float:left;">Around us, it is calm; Hills are covered by mist, Suddenly, the moon shines through the clouds, Graves hold their calm. The white glow of the crosses – heroes are asleep. The shadows of the past circle around, Recalling the victims of battles. Dear mother is shedding tears, The young wife is weeping, All like one are crying, Cursing fate, cursing destiny! Around us, it's calm; The wind blew the fog away, Warriors are asleep on the hills of Manchuria And they cannot hear the Russian tears. Let sorghum's rustling lull you to sleep, Sleep in peace, heroes of the