The map shows quakes of M1.5 and up from the last 90 days, the 0 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 South Zanesville.
Latest earthquakes near South Zanesville
| Mag | Location | Local time | Depth | Distance |
|---|---|---|---|---|
| M2.2 | 7 km S of Nelsonville, Ohio | Aug 31, 2026, 04:06 AM | 18 km | 59 km SSW |
| M3.1 | 3 km S of Pleasant City, Ohio | Apr 24, 2025, 03:14 PM | 6 km | 39 km E |
| M3.1 | 3 km ESE of Buffalo, Ohio | Apr 22, 2025, 04:12 AM | 5 km | 45 km E |
| M3.4 | 1 km WNW of Batesville, Ohio | Jun 02, 2017, 11:08 PM | 2 km | 61 km E |
| M3.4 | 1 km S of McArthur, Ohio | May 24, 2017, 12:24 PM | 10 km | 85 km SSW |
| M3.0 | 5 km W of Graysville, Ohio | Apr 02, 2017, 07:58 AM | 4 km | 70 km ESE |
Earthquakes per year near South Zanesville (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.
What the last year looked like near South Zanesville
Every quake of M1.5 or bigger within 100 km over the last year — 1 in total. A quake of exactly M2.0 counts in the M2.0–3.0 group.
Biggest earthquakes on record near South Zanesville (M4.0 and up, since 1980)
| Mag | Location | Date (UTC) | Distance |
|---|---|---|---|
| No M4.0+ events in the catalog within 100 km since 1980. | |||
Nearby places
Zanesville, OH (5 km) · Pleasant Grove, OH (7 km) · North Zanesville, OH (9 km) · Newark, OH (38 km) · Coshocton, OH (43 km) · Heath, OH (40 km)
USGS data fetched Nov 04, 2026, 01:45 UTC · page built Nov 04, 2026, 01:45 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.