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A glacial erratic is a 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 errare ("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 (16,500…
History, Formation of erratics & Overview
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| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Glacial erratic | is a | glacially deposited rock differing from the type of rock native to the area in which it rests | 0.90 | text |
| Big Rock | instance of | Erratics can range in size from pebbles to large boulders | 0.80 | text |
| Lake Missoula | instance of | which allows quantification of the extent of glacial flooding resulting from ice dam failures which release the waters stored in proglacial lakes | 0.80 | text |
| that created when the ice dam broke during the Missoula floods | instance of | by a flood | 0.80 | text |
| then the erratics are deposited where the ice finally releases its debris load | instance of | by a flood | 0.80 | text |
| Glacial erratic | related to External links | Wiktionary-logo-en-v2 | 0.60 | section |
| Glacial erratic | related to External links | Media | 0.60 | section |
| Glacial erratic | related to External links | Glacial | 0.60 | section |
| Glacial erratic | related to External links | Wikimedia Commons Royal Alberta | 0.60 | section |
| Glacial erratic | related to External links | Museum | 0.60 | section |
| Glacial erratic | see also | Balancing | 0.60 | section |
| Glacial erratic | see also | Puget Sound | 0.60 | section |
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