After the general Late Glacial Maximum a new pulse of glacier advance occurred about 14,850 ka BP. At this point the Golfo Corcovado lobe (ca. 43° S) exceeded any extent it had in the last 30,000 ka BP. Other lobes advanced inside the limits of their earlier Late Glacial Maximum extent. Deglaciation was almost complete after ice-lobes collapsed rapidly after 14,000 ka BP. The Magellanic moorland vegetation around Llanquihue Lake was replaced by North Patagonian Rain Forest including Myrtaceae, Nothofagus dombeyi, Fitzroya cupressoides and Lomatia. Further warming is though to have caused conifer forest, including Fitzroya cupressoides, to lose ground to other vegetation types over much of the lowlands and obtaining its modern discontinuous distribution in the cool heights of the Chilean Coast Range and the Andes.