Analysis of the causes of giant landslide clustering in the upper reaches of the Yellow River since the Holocene

Key Points

• Giant landslide clustering observed in the upper reaches of the Yellow River; geological processes are likely responsible.
• Significant geological processes identified include tectonic activity and erosion patterns that contribute to clustering.
• Observational analysis across geological data from the Holocene period provides crucial insights into landslide behavior.
• Findings highlight the need for further research on landslide prediction and management in vulnerable regions.