CAJ | 학술논문

清水河老牛湾国家地质公园以流水侵蚀、堆积地貌、水体景观为核心景观，辅以黄土地貌景观、古生物化石、地层剖面等地质遗迹景观，同时融合了厚重的历史文化与丰富的人文资源景观。公园内黄土普遍发育，代表了第四纪更新世黄土高原的古地理和古气候环境，可借此研究黄土的成因及黄土高原的形成及环境演变。喇嘛湾河阶地剖面特征，反映它们均属基座阶地，说明清水河地区第四纪以来在新构造运动中曾多次间歇性上升。清水河地区的黄河曲流是在河流下切过程中逐渐侧蚀、演化而成的，具有内生曲流的特点。深切河曲反映了第四纪以来该区发生构造抬升运动，导致河流溯源侵蚀。杨家川瀑布为裂点型瀑布，它在垂向上有规律的分布与新构造运动及溯源侵蚀作用密切相关。黄河支流及古河道遗迹以及河流阶地等地质遗迹，记录了古河流及现代河流地质作用过程，代表了典型的现代及古河流地貌景观。借此可研究现代以及古黄河水流的水动力作用方式及强度，黄河古河道的变迁、区域地质演化史、新构造运动以及该区的古环境变化等问题。
청수하로우만국가지질공완이류수침식、퇴적지모、수체경관위핵심경관，보이황토지모경관、고생물화석、지층부면등지질유적경관，동시융합료후중적역사문화여봉부적인문자원경관。공완내황토보편발육，대표료제사기경신세황토고원적고지리화고기후배경，가차차연구황토적성인급황토고원적형성급배경연변。나마만하계지부면특정，반영타문균속기좌계지，설명청수하지구제사기이래재신구조운동중증다차간헐성상승。청수하지구적황하곡류시재하류하절과정중축점측식、연화이성적，구유내생곡류적특점。심절하곡반영료제사기이래해구발생구조태승운동，도치하류소원침식。양가천폭포위렬점형폭포，타재수향상유규률적분포여신구조운동급소원침식작용밀절상관。황하지류급고하도유적이급하류계지등지질유적，기록료고하류급현대하류지질작용과정，대표료전형적현대급고하류지모경관。차차가연구현대이급고황하수류적수동력작용방식급강도，황하고하도적변천、구역지질연화사、신구조운동이급해구적고배경변화등문제。
Laoniuwan National Geopark ,Qingshuihe County from Inner Mongolia features water erosion , accumulation landforms ,water landscape as the core scenery ,supplemented by loess landscape ,fossils ,the stratigraphic section and other geological heritage landscape ,completed with a blend of profound and rich history and culture human resources landscape .The common development of loess in the park represents the ancient geography and the ancient climate environment of the Quaternary Pleistocene loess plateau ,and can study the genesis of loess and the formation of Loess Plateau and the environment evolution .According to characteristics of Lama Bay terrace profile diagram ,reflecting that they belong to the base terrace ,pointing out in Qingshuihe area since Quaternary in new tectonic movement has repeatedly intermittent rise .Qingshui River area of the Yellow River meandering is in the river cutting in the process of gradually lateral erosion ,evolution and ,with endogenous meandering characteristics .Deep Hequ reflects the tectonic uplift movement since the Quaternary ,resulting in the erosion of the source of the river .The genesis of the Yang Jiachuan falls is a crack type waterfall .This type of waterfall is closely related to the vertical distribution of the vertical and the new tectonic movement and the erosion of the source .Geological relic in the tributaries of the Yellow River and river ancient ruins and river terraces ,represents a typical modern and ancient river landscape ,modern research and ancient Yellow River flow hydrodynamic mode of action and strength ,the changes of ancient river course of the Yellow River ,the regional geological evolution history ,new tectonic movement and the pale environmental change .