By Bryn Hubbard
Box concepts in Glaciology and Glacial Geomorphology is the 1st textual content to supply this crucial info in one complete quantity.
- The function of box facts acquisition within the broader disciplines of glaciology and glacial geomorphology
- Logistical arrangements for fieldwork
- box strategies in glaciology corresponding to investigations on ice and meltwaters
- box strategies in glacial geomorphology starting from investigations on glacial landforms and sediments
- foreign case reviews express every one approach in perform
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Extra resources for Field Techniques in Glaciology and Glacial Geomorphology
Lawson split the facies into three sub-facies: 1. 02 to 55% by volume and ‘includes the relatively pure ice that occurs throughout the stratified facies’ (Lawson, 1979; p. 11). 2. Basal stratified solid sub-facies: This sub-facies is composed of welldefined layers of sediment-rich ice (>50% by volume), commonly characterized by the preservation of internal structures. 3. Basal stratified discontinuous sub-facies: This sub-facies contains irregular aggregates of fine-grained debris. 0 m, and separate units overlapping to form more continuous debris-rich zones.
Consider results 10. Reject hypothesis 11. Accept hypothesis Devise further tests 12. Generalise further or theorise All glaciers, all landforms, some glaciers, some landforms 13. 1 Scientific method and the role of fieldwork in experimental design. Based on ideas presented by Brockie (1972) DESIGNING AND PLANNING FIELD-BASED RESEARCH 19 order to produce generalizations and theories. Finally, in all cases it ought to be possible to make suggestions for further studies that develop the line of enquiry.
L. and Hubbard, B. 2000. Ice crystallographic evolution at a temperate glacier: Glacier de Tsanfleuron, Switzerland. J. Maltman, B. J. Hambrey (eds) Deformation of Glacial Materials, 23–38. The corer is rotated by being driven from the surface by aluminium extension rods that are added as drilling proceeds into the ice. 5). These are driven by a field generator or, if only short cores are required, batteries and solar panels. Once each core section has been cut, indicated at the surface by a drop of one extension rod, rotation ceases and a sharp upward impulse is imparted to the drill to fracture the base of the core.
Field Techniques in Glaciology and Glacial Geomorphology by Bryn Hubbard