Available Weekly Reports
| San Miguel |

23 March-29 March 2011
Servicio Nacional de Estudios Territoriales (SNET) reported that during a survey of the San Miguel crater on 9 and 16 March observers noted pulses of gas rising 200 m from the crater. On 12 March the number and amplitude of earthquakes increased. RSAM values rose the next day to 121 units per day on average, up from normal values around 50 units per day. RSAM values continued to fluctuate during the next few days and reached as high as 319 units on 19 March, 414 units on 20 March, and 234 on 21 March. On 18 and 20 March, local residents felt vibrations and heard minor rumbling. Observations on 25 March indicated that gas plumes rose 100 m from the crater. On 28 March SNET noted that seismicity had gradually decreased during the previous few days, and was as low as 80 RSAM units on 27 March. Access to areas within a 2-km-radius remained restricted.
Sources:
Servicio Nacional de Estudios Territoriales (SNET)
23 March 2011
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Summary of eruption dates and Volcanic Explosivity Indices (VEI).
| Start Date | Stop Date | Eruption Certainty | VEI | Evidence | Activity Area or Unit |
|---|---|---|---|---|---|
| 2002 Jan 16 | 2002 Jan 16 | Confirmed | 1 | Historical | |
| 1997 Dec 31 | Unknown | Confirmed | 1 | Historical | |
| 1995 Jan 12 | 1995 Apr 19 | Confirmed | 1 | Historical | |
| 1985 Nov | 1986 Feb (in or after) | Confirmed | 1 | Historical | |
| 1976 Dec 2 | 1977 Mar 1 | Confirmed | 1 | Historical | |
| 1970 Mar 30 | 1970 Apr 5 | Confirmed | 1 | Historical | |
| 1967 Jan 5 | Unknown | Confirmed | 2 | Historical | |
| 1966 Jul | Unknown | Confirmed | 2 | Historical | |
| 1966 Feb 22 | Unknown | Confirmed | 2 | Historical | |
| 1964 Oct 23 | 1964 Nov | Confirmed | 2 | Historical | |
| 1954 Oct 21 | 1954 Oct 21 | Confirmed | 2 | Historical | |
| 1939 May | 1939 Jul | Confirmed | 2 | Historical | |
| [ 1936 (?) ] | [ Unknown ] | Uncertain | 2 | ||
| 1931 Mar | 1931 Jun | Confirmed | 2 | Historical | |
| 1930 Jan 26 ± 5 days | Unknown | Confirmed | 2 | Historical | |
| 1929 Aug | Unknown | Confirmed | 2 | Historical | |
| 1920 Aug 14 | 1925 | Confirmed | 2 | Historical | |
| 1919 Dec 10 | 1920 Jan | Confirmed | 2 | Historical | |
| 1890 | 1891 | Confirmed | 2 | Historical | |
| 1884 Jan 25 | 1884 Jan 28 ± 1 days | Confirmed | 2 | Historical | NE side of main crater |
| 1882 Dec 5 ± 4 days | Unknown | Confirmed | 2 | Historical | |
| 1867 Dec 14 | 1868 Feb 16 (in or after) | Confirmed | 2 | Historical | WSW flank (1000 m) |
| 1862 Jan | Unknown | Confirmed | 2 | Historical | |
| 1857 Nov | Unknown | Confirmed | 2 | Historical | |
| 1855 Dec | Unknown | Confirmed | 2 | Historical | SSE flank (800 m) |
| [ 1854 ] | [ Unknown ] | Uncertain | 2 | ||
| 1844 Jul 25 | 1848 | Confirmed | 2 | Historical | NNW (1120 m) and upper east flanks |
| 1819 Jul 18 | Unknown | Confirmed | 2 | Historical | SSE flank (400 m; near Los Perolitos) |
| [ 1811 ] | [ Unknown ] | Uncertain | 2 | ||
| [ 1798 (?) ] | [ Unknown ] | Uncertain | 2 | ||
| 1787 Sep 21 | 1787 Sep 23 | Confirmed | 2 | Historical | Summit, north and SE flanks |
| 1769 | Unknown | Confirmed | 2 | Historical | East flank ? |
| 1762 | Unknown | Confirmed | 2 | Historical | NE flank (400 m) |
| 1699 | Unknown | Confirmed | 2 | Historical | SE flank (400 m) |
| 1510 ± 5 years | Unknown | Confirmed | Historical |
The symmetrical cone of San Miguel volcano, one of the most active in El Salvador, rises from near sea level to form one of the country's most prominent landmarks. The unvegetated summit of the 2130-m-high volcano rises above slopes draped with coffee plantations. A broad, deep crater complex that has been frequently modified by historical eruptions (recorded since the early 16th century) caps the truncated summit of the towering volcano, which is also known locally as Chaparrastique. Radial fissures on the flanks of the basaltic-andesitic volcano have fed a series of historical lava flows, including several erupted during the 17th-19th centuries that reached beyond the base of the volcano on the north, NE, and SE sides. The SE-flank lava flows are the largest and form broad, sparsely vegetated lava fields crossed by highways and a railroad skirting the base of the volcano. The location of flank vents has migrated higher on the edifice during historical time, and the most recent activity has consisted of minor ash eruptions from the summit crater.