CAJ | 학술논문

耳阳沟泥石流是甘肃省岷县具有代表性的泥石流沟之一.2010年5月10日，短时强降水导致耳阳沟暴发特大型泥石流.耳阳沟具有支沟泥石流发育、比降大，主沟沟谷宽阔、比降小的特点.泥石流是从其支沟快速冲出，多处堵断主沟又多级溃决、集中冲出形成大规模泥石流，造成严重灾害.
이양구니석류시감숙성민현구유대표성적니석류구지일.2010년5월10일，단시강강수도치이양구폭발특대형니석류.이양구구유지구니석류발육、비강대，주구구곡관활、비강소적특점.니석류시종기지구쾌속충출，다처도단주구우다급궤결、집중충출형성대규모니석류，조성엄중재해.
Eryang Gully debris flow was one of the typical debris flow gullies in Mingxian County. A rainstorm triggered a debris flow hazard in Eryang Gully on May 10, 2010, with the debris flow developing continuously, the lower main gully debris flowbeing wide, and the slope being small. The large debris flow started from the ditch, main trench caused multi-point dam-breakage and the pull trough was incised, causing serious disasters.