- II
- III
- IV
- V
Strongest contour: Moderate (V). Modelled by USGS ShakeMap; contours show where shaking was expected to reach each level, not damage.
People in the shaking
- VModerate7
- IVLight10,000
- IIIWeak178,000
- IIWeak72,000
| Place | Population | Shaking |
|---|---|---|
| Glenorchy | 321 | IV |
| Kelvin Peninsula | 2,000 | IV |
| Milford Sound | 105 | IV |
| Frankton | 2,000 | IV |
| Lake Hawea | 1,000 | III |
| Arrowtown | 3,000 | III |
| Arthurs Point | 1,000 | III |
| Hawea Flat | 543 | III |
Past earthquakes here. A magnitude 6.9 earthquake 132 km se of this event struck Secretary Island, New Zealand on August 10, 1993 (UTC), with estimated population exposures of 5,000 at intensity VI and 2,000 at intensity VII, with no reported fatalities.
Local buildings. Overall, the population in this region resides in structures that are highly resistant to earthquake shaking, though some vulnerable structures exist. The predominant vulnerable building types are reinforced masonry and unreinforced brick with timber floor construction.
Population and intensity modelled by USGS PAGER. Estimates, not a count of people affected.
U.S. Geological Survey
Terremoto preserves this event snapshot for a stable public link. USGS remains the authoritative source for revisions and scientific details. Shaking contours and population estimates come from USGS ShakeMap and PAGER, which revise them as more data arrives.