RSS feed source: Volcano Discovery.com--Global earthquake monitor

3 km (2 mi)

S of epicenter

Lagunillas

(pop: 522)

IV: Light

Santiago Pinotepa Nacional, Estado de Oaxaca 10 km (6 mi)

E of epicenter

Lo de Candela

(pop: 538)

IV: Light

Santiago Pinotepa Nacional, Estado de Oaxaca 15 km (9 mi)

NW of epicenter

Santiago Llano Grande

(pop: 1,880)

IV: Light

Estado de Oaxaca 15 km (10 mi)

S of epicenter

Corralero

(pop: 1,740)

III: Weak

Santiago Pinotepa Nacional, Estado de Oaxaca 17 km (11 mi)

W of epicenter

Santo Domingo Armenta

(pop: 2,580)

III: Weak

Estado de Oaxaca 19 km (12 mi)

E of epicenter

Pinotepa Nacional

(pop: 29,600)

III: Weak

Estado de Oaxaca 23 km (14 mi)

NW of epicenter

Cuajinicuilapa

(pop: 10,300)

III: Weak

Estado de Guerrero 24 km (15 mi)

E of epicenter

San Pedro Jicayan

(pop: 4,710)

III: Weak

San Pedro Jicayan, Estado de Oaxaca 26 km (16 mi)

NE of epicenter

San Antonio Tepetlapa

(pop: 2,620)

III: Weak

Estado de Oaxaca 28 km (17 mi)

N of epicenter

San Juan Cacahuatepec

(pop: 4,240)

III: Weak

Estado de Oaxaca 32 km (20 mi)

W of epicenter

San Nicolas

(pop: 3,270)

III: Weak

Cuajinicuilapa, Estado de Guerrero 33 km (20 mi)

N of epicenter

Huixtepec

(pop: 3,370)

III: Weak

Ometepec, Estado de Guerrero 33 km

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Background:

Volcán Popocatépetl, whose name is the Aztec word for smoking mountain, towers to 5426 m 70 km SE of Mexico City to form North America’s 2nd-highest volcano.  The glacier-clad stratovolcano contains a steep-walled, 250-450 m deep crater.  The generally symmetrical volcano is modified by the sharp-peaked Ventorrillo on the NW, a remnant of an earlier volcano. 
At least three previous major cones were destroyed by gravitational failure during the Pleistocene, producing massive debris-avalanche deposits covering broad areas south of the volcano.  The modern volcano was constructed to the south of the late-Pleistocene to Holocene El Fraile cone.  Three major plinian eruptions, the most recent of which took place about 800 AD, have occurred from Popocatépetl since the mid Holocene, accompanied by pyroclastic flows and voluminous lahars that swept basins below the volcano.  Frequent historical eruptions, first recorded in Aztec codices, have occurred since precolumbian

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