粗语
发表于 2025-3-30 09:44:18
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肌肉
发表于 2025-3-30 15:48:14
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有组织
发表于 2025-3-30 18:24:59
Geomorphology of the Adwa Districtterm landscape evolution from the Late Proterozoic to the Quaternary. Two landscape features of the Adwa district exemplify the control of tectonic uplift and erosion, often in a feedback loop: the plateau landscape and river incision. The plateau landscape developed upon metamorphic, sedimentary an
alabaster
发表于 2025-3-30 23:36:13
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有恶臭
发表于 2025-3-31 01:13:41
Gully Development in the Tigray Highlandsment, where intense rainfalls challenge the physical integrity of the landscape. Over the last two centuries, three major phases in the hydrological regime of the region could be distinguished. In the first phase, between 1868 (or earlier) and ca. 1965, the relatively stable gully channels showed an
裹住
发表于 2025-3-31 06:52:07
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altruism
发表于 2025-3-31 10:18:15
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缝纫
发表于 2025-3-31 13:50:53
Sediment Yield Variability at Various Spatial Scales and Its Hydrological and Geomorphological Impacile River Basin. SY data collected using reservoir sediment surveys or runoff and suspended sediment concentration (SSC) measurements at river gauging stations in the framework of different programs were compiled, screened, and used for our analysis. A large spatial variation in area-specific SY (SS
anniversary
发表于 2025-3-31 19:03:38
Climatic and Hydrologic Changes in Northern Ethiopia in the last 3,500 Years: Evidence from the Geomrved along the lake margins provide a detailed archive of the climate history of East Africa over the past 3,500 years. These successions are represented by colluvial/stromatolitic deposits and palustrine, deltaic, and fluvial sediments along the northern and southern coasts, respectively. During th
半身雕像
发表于 2025-4-1 00:30:38
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