File:2003-11-27_Northerner_boots_in_mud.jpg · Wikimedia Commons · See Wikimedia Commons
thumb|upright=1.35|A pair of muddy Wellington boot|Wellington boots thumb|Gamo mud volcano in Tokamachi, Japan Mud (, or Middle Dutch) is loam, silt or clay mixed with water. Mud is usually formed after rainfall or near water sources. Ancient mud deposits hardened over geological time to form sedimentary rock such as shale or mudstone (generally called lutites). When geological deposits of mud are formed in estuaries, the resultant layers are termed bay muds. Mud has also been used for centuries as a construction resource for mostly houses and also used as a binder. An Old English word for it
Mud is a mixture of loam, silt, or clay combined with water, typically formed after rainfall or near water sources. Over geological time, ancient mud deposits have hardened into sedimentary rocks like shale and mudstone, and humans have used mud for centuries as a building material and binder for construction.
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Wikidata facts
- Subclass of
- clastic sediment
- Image
- Yellowstone mud pot p1090998.jpg
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- described by source
- Explanatory Dictionary of the Living Great Russian Language
- on focus list of Wikimedia project
- Wikipedia:Vital articles/Level/4
- Commons category
- Mud
- Commons gallery
- Mud
- OpenStreetMap tag
- surface=mud
- exact match
- purl.obolibrary.org/obo/ENVO_01000001
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Article · 中文
泥(英語:Mud)是與水混合的土壤(soil)、壤土(Loam)、淤泥(英語:silt)或黏土(clay)。它通常在降雨後或水源附近形成。古老的泥漿沉積物隨著地質時間的推移而硬化,形成沉積岩,例如頁岩或泥岩。當在河口形成泥質地質沉積物時,形成的層被稱為。
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