The map shows quakes of M1.5 and up from the last 90 days, the 3 biggest on record, and always the very latest quake — even if it was smaller than M1.5. The list below can include smaller ones the map leaves out. Tap any dot for details.
In the last 30 days, 0 earthquakes of M1.5 or bigger were recorded within 100 km of Linton Hall. The biggest quake on record near Linton Hall — records go back to 1980 — was the M5.8 of Aug 23, 2011, 17:51 UTC: 11 km SSW of Mineral, Virginia.
Latest earthquakes near Linton Hall
| Mag | Location | Local time | Depth | Distance |
|---|---|---|---|---|
| M3.0 | 3 km NE of Ranson, West Virginia | Jan 17, 2016, 02:12 PM | 5 km | 66 km NNW |
| M4.5 | 8 km SW of Mineral, Virginia | Aug 25, 2011, 01:07 AM | 7 km | 97 km SSW |
| M4.2 | 11 km SSW of Mineral, Virginia | Aug 23, 2011, 08:04 PM | 0 km | 100 km SSW |
| M5.8 | 11 km SSW of Mineral, Virginia | Aug 23, 2011, 01:51 PM | 6 km | 100 km SSW |
Earthquakes per year near Linton Hall (M3.0 and up, within 100 km)
M3.0–3.9 M4.0+
Each bar is one year; taller means more quakes (M3.0 and up). The dark red part is the bigger ones (M4.0+), counted inside the number above each bar — not added on top. These may be felt, depending on how far away and how deep they are. 2026 is not a full year yet — it only counts up to today. Source: USGS Earthquake Catalog.
The 3 biggest earthquakes on record near Linton Hall (M4.0 and up, since 1980)
| Mag | Location | Date (UTC) | Distance |
|---|---|---|---|
| M5.8 | 11 km SSW of Mineral, Virginia | Aug 23, 2011, 17:51 UTC | 100 km |
| M4.5 | 8 km SW of Mineral, Virginia | Aug 25, 2011, 05:07 UTC | 97 km |
| M4.2 | 11 km SSW of Mineral, Virginia | Aug 24, 2011, 00:04 UTC | 100 km |
Nearby places
New Baltimore, VA (13 km) · Independent Hill, VA (18 km) · Warrenton, VA (20 km) · Dale City, VA (27 km) · Montclair, VA (26 km) · Culpeper, VA (49 km)
USGS data fetched Nov 03, 2026, 18:45 UTC · page built Nov 03, 2026, 18:45 UTC. How to read this page: recent-window counts cover M1.5+ events within 100 km; the 10-year layer is based on M3.0+ and the history layer on M4.0+ since 1980. Recording completeness varies by era and region — small quakes from early decades are under-recorded, so “no record” does not prove “never happened”. Depths are relative to sea level and can be slightly negative for shallow events in elevated terrain. Method: data & methodology.