Completed catalogue assessment

Eligibility decision: Include · Include
Assessment date: 28 September 2026
Decision reason: Original source identity and relevant content established; exact unsupported metadata replaced and evidential limits recorded.
Metadata corrections: {"validation_status":"agency_reviewed_event_solution","last_updated":"","description":"USGS event us7000tbwb is classified as a landslide with origin 02:52:10 UTC, magnitude 5.2 of type ms_vx, and point coordinates 85.515° E, 28.271° N at an assigned depth of 0 km.","uncertainty_summary":"The original response does not establish location accuracy within 5 km or origin-time accuracy within 1 second. A reported zero depth and precise timestamp are not independent accuracy estimates.","limitations":"The event bulletin is a seismic source estimate, not a direct measurement of detached volume, flow velocity, or failure mechanism. Current response retrieved 28 September; inventory membership at the 24 September cutoff is distinct from the current dynamic endpoint content.","reviewed_on":"2026-09-28","current_status":"eligibility_assessed"}

Identity and coverage

Catalogue identifier: res-7b19a4e2-8e12-4f39-9d51-c0e8125439a1
Original-title language: English
English-title status: Not applicable
Persistent identifier: us7000tbwb
Resource version: Version 1
Publication date: 26 August 2026
Last updated: Not stated
Metadata reviewed: 28 September 2026
Language: English
Geographic coverage: Northern flank of Langtang Lirung, Rasuwa District, Nepal
Bounding box (WGS 84): [85.515,28.271,85.515,28.271]
Temporal coverage: 26 August 2026; Event
Themes: Seismology, Mass Movement, Initiation Timing, Landslide Seismology, Geophysics

Production method: Automated seismic wave detection from regional and global broadband stations, reviewed and classified by USGS National Earthquake Information Center (NEIC) analysts as a landslide mass-movement signal.
Provenance: Published directly by the USGS Earthquake Hazards Program via the ComCat API.
Validation: Agency Reviewed Event Solution
Uncertainty: The original response does not establish location accuracy within 5 km or origin-time accuracy within 1 second. A reported zero depth and precise timestamp are not independent accuracy estimates.
Limitations: The event bulletin is a seismic source estimate, not a direct measurement of detached volume, flow velocity, or failure mechanism. Current response retrieved 28 September; inventory membership at the 24 September cutoff is distinct from the current dynamic endpoint content.