VolcanoYT

Disaster Monitoring

Volcanic Ash Advisory

Fuego

Mon, 03 Aug 2026 20:53:00 GMT
Raw Output
FVXX20 at 20:56 UTC, 03/08/26 from KNES
VA ADVISORY
DTG: 20260803/2053Z

VAAC: WASHINGTON

VOLCANO: FUEGO 342090
PSN: N1428 W09052

AREA: GUATEMALA

SOURCE ELEV: 12346 FT AMSL

ADVISORY NR: 2026/900

INFO SOURCE: GOES-19. WEBCAM. NWP MODELS. 

ERUPTION DETAILS: FRQT VA EMS OBS

OBS VA DTG: 03/2030Z

OBS VA CLD: SFC/FL140 N1444 W09134 - N1438 W09102
- N1429 W09052 - N1427 W09053 - N1425 W09107 -
N1426 W09119 - N1423 W09132 - N1434 W09138 -
N1444 W09134 MOV NW 5KT 

FCST VA CLD +6HR: 04/0230Z SFC/FL140 N1441 W09144
- N1428 W09052 - N1427 W09052 - N1426 W09147 -
N1441 W09144 

FCST VA CLD +12HR: 04/0830Z SFC/FL140 N1454
W09138 - N1428 W09052 - N1427 W09053 - N1443
W09145 - N1454 W09138 

FCST VA CLD +18HR: 04/1430Z SFC/FL140 N1435
W09146 - N1429 W09052 - N1427 W09052 - N1421
W09146 - N1435 W09146 

RMK: VA EMS OBSD IN WEBCAM AND STLT IMG EXTG
APPRX 45 NM WNW AND W FM SUMMIT. WNW MVMT EXP TO
SHIFT NW BY T+12 HRS AND W BY T+18 HRS.
MVMT AND HGT BASED ON WEBCAM, STLT OBS AND NWP
MDLS. ...BERTALAN

NXT ADVISORY: WILL BE ISSUED BY 20260804/0300Z
Fuego

Fuego

Guatemala
Level 4

Volcán Fuego, one of Central America's most active volcanoes, is also one of three large stratovolcanoes overlooking Guatemala's former capital, Antigua. The scarp of an older edifice, Meseta, lies between Fuego and Acatenango to the north. Construction of Meseta dates back to about 230,000 years and continued until the late Pleistocene or early Holocene. Collapse of Meseta may have produced the massive Escuintla debris-avalanche deposit, which extends about 50 km onto the Pacific coastal plain. Growth of the modern Fuego volcano followed, continuing the southward migration of volcanism that began at the mostly andesitic Acatenango. Eruptions at Fuego have become more mafic with time, and most historical activity has produced basaltic rocks. Frequent vigorous historical eruptions have been recorded since the onset of the Spanish era in 1524, and have produced major ashfalls, along with occasional pyroclastic flows and lava flows.

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