By Helen Babbs
From deep iciness to overdue autumn, from east to west, Adrift takes the reader on a journey of the folk, politics, background and flora and fauna of London’s canals and rivers. mixing nature writing, social commentary and memoir, Helen Babbs invitations you on an eye-opening trip right into a diversified facet of the town. From Walthamstow Marsh within the east to Uxbridge within the west, Helen Babbs trips alongside London’s waterways on a canal boat referred to as Pike, placing down roots for 2 weeks at a time ahead of relocating on. Taking within the River Lea and the Lee Navigation, the Regent’s Canal and the Grand Union, she explores the London panorama in all its guises: marshland, desolate tract, urban centre and suburb. Adrift charts a 12 months of Helen’s existence on Pike, exploring the alterations wreaked by means of the seasons in addition to by means of builders, and recounting the sensible trials of residing aboard. it's a tale of mapping and discovery, of break out and opting out, but additionally of constructing connections and discovering domestic. simply because the coots and cormorants steer clear of the detritus of a giant urban, so too does Helen wend during the good looks and the airborne dirt and dust to bare an intimate and weird portrait of London and of existence.
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Additional info for Adrift: A Secret Life of London's Waterways
It forms cliﬀs with 10–30 m in relative elevation. There is a ﬂexure concealed by sediment oﬀ the Nagahama, but the activity after the K-Ah tephra is never recognized. Central Flexure forms saddle topography separating the northern and middle basins. It lasts about 6 km in the north and south, and shows convex in the west. The ﬂexure is elevated in the western side. Its hanging wall is dipped to the west showing small deformation (> Fig. 5-C). The amounts of displacement are 12 m at the bottom surface, 18 m at the K-Ah tephra, 40 m at the AT tephra, and 170 m at TS surface (the base of the Biwako Clay Bed, dating to about 400,000 years ago).
6 Ma, and ultimately the rest ﬁlled in as well. Reduction and Disappearance of the Lake After the ﬁlling in and disappearance of Paleo-lake Ayama, there were small ponds and/or marshes to the southeast and south of the present lake, which are collectively called Paleo-lakes Gamo (corresponding to the period of deposition of the Gamo Formation). 2 Geological History of Lake Biwa ⊡ Fig. 4 Pliocene to Pleistocene formations of central Honshu Island (Simplified from Japan Association for Quaternary Research 1987).
Southwestern Japan, thereafter, started to rotate clockwise while northeastern Japan started to rotate counterclockwise to reach the present location about 14 million years ago, as shown in > Fig. 2. During the Late Paleogene to the Early Miocene, a large rift valley was formed between the continent and the Japanese archipelago (Otofuji and Matsuda 1984). Wide distribution of freshwater sediments indicates that several large lakes were formed there. Such a large-scale geological activity seems to have generated new environments in the marginal part of the continent, diﬀerent from those in inland areas.
Adrift: A Secret Life of London's Waterways by Helen Babbs