er⋅rat⋅ic
[i-rat-ik]
| 1. | deviating from the usual or proper course in conduct or opinion; eccentric; queer: erratic behavior. |
| 2. | having no certain or definite course; wandering; not fixed: erratic winds. |
| 3. | Geology. noting or pertaining to a boulder or the like carried by glacial ice and deposited some distance from its place of origin. |
| 4. | (of a lichen) having no attachment to the surface on which it grows. |
| 5. | an erratic or eccentric person. |
| 6. | Geology. an erratic boulder or the like. |
Based on the Random House Dictionary, © Random House, Inc. 2009.
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Copyright © 2009 by Houghton Mifflin Company.
Published by Houghton Mifflin Company. All rights reserved.
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Erratic
Er*rat"ic\, a. [L. erraticus, fr. errare to wander: cf. F. erratique. See Err.]1. Having no certain course; roving about without a fixed destination; wandering; moving; -- hence, applied to the planets as distinguished from the fixed stars. The earth and each erratic world. --Blackmore. 2. Deviating from a wise of the common course in opinion or conduct; eccentric; strange; queer; as, erratic conduct. 3. Irregular; changeable. "Erratic fever." --Harvey. Erratic blocks, gravel, etc. (Geol.), masses of stone which have been transported from their original resting places by the agency of water, ice, or other causes. Erratic phenomena, the phenomena which relate to transported materials on the earth's surface.Erratic
Er*rat"ic\, n. 1. One who deviates from common and accepted opinions; one who is eccentric or preserve in his intellectual character. 2. A rogue. [Obs.] --Cockeram. 3. (Geol.) Any stone or material that has been borne away from its original site by natural agencies; esp., a large block or fragment of rock; a bowlder. Note: In the plural the term is applied especially to the loose gravel and stones on the earth's surface, including what is called drift.Cite This Source
erratic
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Main Entry: er·rat·ic
Pronunciation: ir-'at-ik
Function: adjective
1 : characterized by lack of consistency, regularity, or uniformity
2 : deviating from what is ordinary or standard
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erratic
glacier-transported rock fragment that differs from the local bedrock. Erratics may be embedded in till or occur on the ground surface and may range in size from pebbles to huge boulders weighing thousands of tons. The distance of transportation may range from less than 1 km (0.6 mile) to more than 800 km (500 miles); those transported over long distances generally consist of rock resistant to the shattering and grinding effects of glacial transport. Erratics composed of unusual and distinctive rock types can be traced to their source of origin and serve as indicators of the direction of glacial movement. Studies making use of such indicator erratics have provided information on the general origins and flow paths of the major ice sheets and on the locations of important mineral deposits. Erratics played an important part in the initial recognition of the last ice age and its extent. Originally thought to be transported by gigantic floods or by ice rafting, erratics were first explained in terms of glacial transport by the Swiss-American naturalist and geologist J.L.R. Agassiz in 1840.
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