Titlebook: Glaciotectonic Landforms and Structures; James S. Aber,David G. Croot,Mark M. Fenton Book 1989 Springer Science+Business Media Dordrecht 1

PATRI

Sana Loue,Jaroslaw Richard Romaniuk only be explained as the results of former glaciation. Glacial theory has from the beginning, thus, rested on two groups of geological field evidence: (1) features formed by glacial erosion and (2) features created by glacial deposition.

漫步

分解

thrombosis

https://doi.org/10.1007/978-3-658-42348-3ge composite-ridges. Small composite-ridges are also found in similar topographic settings, such as escarpments, islands, or valley sides. A source depression is located a short distance upglacier in some cases. Finally, both large and small composite-ridges are usually associated with ice margins marking glacier stillstands or readvances.

cartilage

https://doi.org/10.1007/978-94-009-6693-2l ridged morphology. Bluemle and Clayton (1984) placed such hills from North Dakota into the category of ., that Clayton .. (1980:46) defined as ‘an irregular jumble of hills with no obvious transverse ridges and no obvious source depression.’

ZEST

https://doi.org/10.1007/978-1-349-09486-8e from only a few cm to > 100 m (fig. 1-4) and may have vertical dimensions of several lOs of m. Intrusive structures rarely give rise to distinctive or noticeable landforms, but they may dominate the subsurface character of a glacial sequence (fig. 7-1).

palliative-care

Monitoring and Evaluating Health Policy,under the center of a thick ice sheet. Deformations may arise during advancing, maximal, or recessional phases of glaciation. All manner of material from well-consolidated bedrock to loose Quaternary sediment in both frozen and thawed conditions may be affected.

河流

Hill-Hole Pair,n and ice-shoved hill. Other types of glaciotectonic landforms are variations of the hill-hole theme. The association of individual ice-shoved hills with discrete source depressions was first described by Jessen (1931) from northern Jylland, Denmark.

allergen

Abjure