However, for smaller productions (e.g. corporate and event videography), a videographer often works alone with a single-camera setup or in the case of a multiple-camera setup, as part of a larger television crew with lighting technician, grips and sound operators.
Note the moraines around the margins, and the folds formed by compression as the debris-rich ice enters the flat lowland. The folds are clear evidence that plastic deformation is a strong component of glacial flow. Date taken Feb.11, 2000.hen the final ice melted, these deposits became positive features; channels became ridges and depressions became hills. Hummocky moraine, formed over a large region of stagnant ice (fig. 14) may contain a mixture of irregular and interstratified till and meltwater deposits.
Moraines are formed from debris previously carried along by a glacier and normally consist of somewhat rounded particles ranging in size from large boulders to minute glacial flour. Lateral moraines are formed at the side of the ice flow and terminal moraines at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines, till-covered areas with irregular topography, and medial moraines which are formed where two glaciers meet.