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Erratum

Published online by Cambridge University Press:  08 September 2017

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Correction
Information
Journal of Glaciology , Volume 48 , Issue 161 , 2002 , pp. 341 - 342
Copyright
Copyright © International Glaciological Society 2002

Li Yingkui, Liu Gengnian and Cui Zhijiu. 2001. Longitudinal varitions in cross-section morphology along a glacial valley: a case-study from the Tien Shan, China. J.Glacial., 47(157), 243–250.

Incorrect versions of Figures 4, 6 and 8 were published. Please replace them with those that follow:

Fig. 4. Method of smoothing of valley cross-sections before calculating VWDR values: (1) interpolate across the valley bottom if the valley has been incised by fluvial or other processes in postglacial time; (2) interpolate beneath talus or moraines on valley sides.

Fig. 6. Classification of glacial valleys. A, B, simple valleys; C, compound valley. (1) upper simple-valley section; (2) confluent section; (3) lower simple section.

Fig. 8. Longitudinal variation of trimline altitude, In m and n along some compound valleys. The short vertical arrows in each panel show the locations of confluences, (a) Daxigou valley; (b) Glacier No. 8–Daxigou valley; (c) Akesudangha–Ayoutuaiken valley; (d) Yawuertuaiken–Ayoutuaiken valley.

Figure 0

Fig. 4. Method of smoothing of valley cross-sections before calculating VWDR values: (1) interpolate across the valley bottom if the valley has been incised by fluvial or other processes in postglacial time; (2) interpolate beneath talus or moraines on valley sides.

Figure 1

Fig. 6. Classification of glacial valleys. A, B, simple valleys; C, compound valley. (1) upper simple-valley section; (2) confluent section; (3) lower simple section.

Figure 2

Fig. 8. Longitudinal variation of trimline altitude, In m and n along some compound valleys. The short vertical arrows in each panel show the locations of confluences, (a) Daxigou valley; (b) Glacier No. 8–Daxigou valley; (c) Akesudangha–Ayoutuaiken valley; (d) Yawuertuaiken–Ayoutuaiken valley.