Significant earthquakes of 1990

May 20, 1990 Earthquake: Nakura, Juba, Maya, Uganda, South Sudan

May 20, 1990 · M7.1 · 31 deaths

A magnitude 7.1 earthquake struck Nakura, Juba, Maya, Uganda, South Sudan on May 20, 1990 at 02:22:01 UTC, 15 km below the surface. It killed 31 people.

Map

Where it struck, with the other significant earthquakes within 200 km. Circles are sized and colored by magnitude; select one for its page.

The earthquake

Date
May 20, 1990
Time
02:22:01 UTC
Place
Nakura, Juba, Maya, Uganda, South Sudan
Magnitude
7.1 (Ms)
Focal depth
15 km (9 mi)
Tsunami
None recorded
Epicenter
5.121° N, 32.145° E

The toll

Deaths
31
Damage
Limited (under about $1 million)
Houses damaged
Some (about 51 to 100)

Where the literature gives no number, NCEI records a description on a scale of 1 to 4, printed here in its words. Damage is in millions of US dollars of the year of the event, not adjusted for inflation.

What the record says

NCEI’s account, from the sources it cites.

May 20, 1990, Sudan. Some buildings damaged in the Juba area. Also damage in the Moyo area, Uganda. Felt in the Nakura area, Kenya and in Uganda. (reference #1053)

May 19, 1990 [probably describing May 20, 1990 event], Sudan. 31 killed. (reference #1250)

Several large earthquakes occurred in the south of the Sudan (now South Sudan) in May and July 1990. On 20 May 1990, a large earthquake of magnitude M7.2, shook the region located about 1120 km south of Khartoum and 100 km northeast of Juba, in the Mongola area. It was reported that 31 people lost their lives during this earthquake (http://earthquakes.findthedata.org/l/4608/Sudan- Juba-Maya-Uganda-Nakura). On 24 May 1990 another earthquake of magnitude M7.1 occurred in the same region, about 25 km south of the first one. This earthquake caused more substantial damage to private housing and government institutions than the first one but no loss of life was reported. Minor cracking in walls of some older buildings was observed in Juba. Most of the impact of the event fell on uninhabited areas. The focal mechanism of the main shock (20 May 1990) shows left-lateral strike-slip faulting (Gaulon et al., 1992, Girdler and McConnell, 1994). One of the nodal planes is parallel to the Aswa fault zone, a major Proterozoic tectonic feature. A line connecting the epicentres of the main events of May and July also strikes in the same direction. The rupture occurred in at least three steps, affecting a zone roughly 50 km long. However, the focal mechanism of the 20 May 1990 event was found to be different from the aftershocks, which all occurred on normal faults indicating a complicated tectonic regime in the epicentral area (Foster and Jackson, 1998). (reference #13028)

Other significant earthquakes nearby

Within 200 km, the deadliest first.

More

Significant earthquakes of 1990The 1900sEvery quake the USGS located in 1990Recent earthquakes near hereThis day in weather history

Sources

Significant earthquakes from NOAA’s National Centers for Environmental Information, Global Historical Hazard Database, cited as NCEI/WDS, doi:10.7289/V5PN93H7. Public domain. Read 2026-09-24. NCEI earthquake 5237.