Erratic Lake
Erratic may refer to: * Erratic, a project of music artist Jan Robbe * Glacial erratic, a piece of rock that differs from the size and type of rock native to the area in which it rests * Erratic ant The erratic ant (''Tapinoma erraticum'') is a species of dolichoderine ant first described in 1789 by Latreille. This species ranges throughout Central Europe from the mountains of south Italy to north Germany. It is present in coastal areas o ...

Jan Robbe
Jan Robbe (born 14 June 1980 in Ghent, Belgium), otherwise known by his music project aliases Atomhead, Erratic, UndaCova and Diagnostic, is an electronic music artist. He founded the experimental netlabel Entity in 2003 with friend Nico de Gols (aka Kaebin Yield). Jan Robbe is known for expressing various musical styles under different pseudonyms. ''Atomhead'' and ''UndaCova'', his two most prominent projects, focus on fractured industrial beats and densely textured DSP sound design techniques, whereas ''Erratic'' is a vehicle for pursuing more minimal long-form ambiental directions. The most recent (2018) ''Diagnostic'' project explores experimental sound design, glitch and noise structures, combining digital and modular synthesis. Robbe has released music on distinguished labels such as Dyslexic Response and Hangars Liquides, and collaborated with artists who operate in similar aesthetic domains, including La Peste, Neurocore, Subskan and Xanopticon. Besides his activities as ...
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Glacial Erratic
A glacial erratic is glacially deposited rock differing from the type of rock native to the area in which it rests. Erratics, which take their name from the Latin word ' ("to wander"), are carried by glacial ice, often over distances of hundreds of kilometres. Erratics can range in size from pebbles to large boulders such as Big Rock () in Alberta. Geologists identify erratics by studying the rocks surrounding the position of the erratic and the composition of the erratic itself. Erratics are significant because: *They can be transported by glaciers, and they are thereby one of a series of indicators which mark the path of prehistoric glacier movement. Their lithographic origin can be traced to the parent bedrock, allowing for confirmation of the ice flow route. *They can be transported by ice rafting. This allows quantification of the extent of glacial flooding resulting from ice dam failure which release the waters stored in proglacial lakes such as Lake Missoula. Erratics ...
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