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.
Hummocky cross-stratification from the Arisag Formation (Silurian), Nova Scotia. Hummocky cross-stratification is a type of sedimentary structure found in sandstones. It is a form of cross-bedding usually formed by the action of large storms, such as hurricanes.It takes the form of a series of smile-like shapes, crosscutting each other.istory [edit]. The name was introduced by Harms et al. in 1975. Before this time, these structures were recognized under many different names. When hummocky cross-stratification was founded, it was originally given the name âtruncated wave-ripple laminae,â by Campbell (1966, 1971).