WordNet
- a steep artificial slope in front of a fortification (同)escarp, scarp, protective embankment
- a long steep slope or cliff at the edge of a plateau or ridge; usually formed by erosion (同)scarp
- soft mild Italian cream cheese
- mark with a scar; "The skin disease scarred his face permanently" (同)mark, pock, pit
- a mark left (usually on the skin) by the healing of injured tissue (同)cicatrix, cicatrice
PrepTutorEJDIC
- 急傾斜,急坂
- (地殻の断層・亀裂などによる)断崖(だんがい) / 急斜面をめぐらした城(とりで)
- とんずらする,(特に)食い逃げする
- (皮膚の)『傷跡』;(物の表面の)傷跡 / 心の傷跡,痛手;(名誉などを傷つける)汚点 / (植物の茎などに残る)葉印,葉痕(ようこん) / …‘に'傷跡を残す / 〈傷などが〉傷跡を残す《+『over』》
Wikipedia preview
出典(authority):フリー百科事典『ウィキペディア(Wikipedia)』「2013/01/29 07:10:17」(JST)
[Wiki en表示]
Scarp may refer to:
Landforms and geology
- Cliff, a significant vertical, or near vertical, rock exposure
- Escarpment, a steep slope or long rock that occurs from erosion or faulting and separates two relatively level areas of differing elevations
- Scarp face, the surface of the steep slope of an escarpment
- Fault scarp, the topographic expression of faulting attributed to the displacement of the land surface by movement along faults
Other
- Scarp, Scotland, an island in the Outer Hebrides of Scotland
- Counterscarp and Scarp, the outer and inner sides of a ditch used in fortifications
- SS-9 Scarp, the NATO reporting name for the R-36 ICBM
See also
English Journal
- Identification of a putative quantitative trait nucleotide in guanylate binding protein 5 for host response to PRRS virus infection.
- Koltes JE1, Fritz-Waters E2, Eisley CJ3,4, Choi I5, Bao H6, Kommadath A7, Serão NV8, Boddicker NJ9, Abrams SM10, Schroyen M11, Loyd H12, Tuggle CK13, Plastow GS14, Guan L15, Stothard P16, Lunney JK17, Liu P18, Carpenter S19, Rowland RR20, Dekkers JC21, Reecy JM22.
- BMC genomics.BMC Genomics.2015 May 28;16:412. doi: 10.1186/s12864-015-1635-9.
- BACKGROUND: Previously, we identified a major quantitative trait locus (QTL) for host response to Porcine Respiratory and Reproductive Syndrome virus (PRRSV) infection in high linkage disequilibrium (LD) with SNP rs80800372 on Sus scrofa chromosome 4 (SSC4).RESULTS: Within this QTL, guanylate bindin
- PMID 26016888
- Contrasting taxonomic and phylogenetic diversity responses to forest modifications: comparisons of taxa and successive plant life stages in South African scarp forest.
- Grass I1, Brandl R2, Botzat A3, Neuschulz EL4, Farwig N1.
- PloS one.PLoS One.2015 Feb 26;10(2):e0118722. doi: 10.1371/journal.pone.0118722. eCollection 2015.
- The degradation of natural forests to modified forests threatens subtropical and tropical biodiversity worldwide. Yet, species responses to forest modification vary considerably. Furthermore, effects of forest modification can differ, whether with respect to diversity components (taxonomic or phylog
- PMID 25719204
- Computational modeling suggests dimerization of equine infectious anemia virus Rev is required for RNA binding.
- Umunnakwe CN1,2, Loyd H3, Cornick K4, Chavez JR5, Dobbs D6,7, Carpenter S8.
- Retrovirology.Retrovirology.2014 Dec 23;11(1):115. doi: 10.1186/s12977-014-0115-7.
- BACKGROUND: The lentiviral Rev protein mediates nuclear export of intron-containing viral RNAs that encode structural proteins or serve as the viral genome. Following translation, HIV-1 Rev localizes to the nucleus and binds its cognate sequence, termed the Rev-responsive element (RRE), in incomplet
- PMID 25533001
Japanese Journal
- 空から見る日本の地すべり地形シリーズ(32)飛驒山脈北部・朝日岳南面に認められる重力性山体変形
- 八木 浩司,井口 隆
- 日本地すべり学会誌 : 地すべり = Journal of the Japan Landslide Society : landslides 50(6), 288-290,図巻頭2p, 2013-11
- NAID 40019899989
- On-land active thrust faults of the Nankai–Suruga subduction zone: The Fujikawa-kako Fault Zone, central Japan
- Lin Aiming,Iida Kenta,Tanaka Hideto
- Tectonophysics 601, 1-19, 2013-08
- … and iv) the 864–865 AD Jogan lava flow is displaced by 2–4 m vertically along the scarp at the northeastern end of the fault zone. …
- NAID 120005307000
- 今泉 文寿,SIDLE Roy C.,外狩 麻子,島村 誠
- 地形 34(2), 129-146, 2013-04-25
- … Our observation results showed that soil creep was active above the head scarp of the landslide, whereas soil creep was relatively inactive around the sides of the landslide. … Soil creep mainly contributes to infilling of the landslide scar via sediment inputs from the slope above the head scarp rather than along the flanks of the landslide. …
- NAID 110009612376
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Related Pictures
![Picture 1: Fault scarp, Zhangye thrust](https://1mg.info/0/3/m/2059.jpg)
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![Triangular Fault Scarps](https://1mg.info/0/3/m/2061.jpg)
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![Normal-Fault Scarp](https://1mg.info/0/3/m/2065.jpg)