Expanded monitoring efforts and explosive hydrothermal event in July 2009

Previously reported activity from Azufral included seismic swarms in 1971 (CSLP 43-71) and fluctuating conditions within the crater lake, Laguna Verde during July-August 1990 (BGVN 15:08) (figure 1). In this report, we highlight explosive hydrothermal activity that occurred during July-August 2009. We also provide observations of Azufral's hydrothermal and fumarolic activity and review monitoring efforts that expanded since 2005.

Fumarolic activity within Azufral's largest crater had long been observed by Colombia's earliest inhabitants and investigators including Alexander von Humboldt in the 1800s (Yudilevich Levy, 2004). In one of his many journals, Diario VII "Viaje de Pasto a Quito," this naturalist noted the rugged morphology of the edifice, describing it as a volcano that had broken apart; similar in appearance to Sotará, a volcano he had already visited. At the time of his visit in December 1801, there were significant deposits of sulfur and strong gas emissions within the crater, particularly around the largest crater lake (he noted that there were several craters in the complex, the largest now known as Laguna Verde).

"Una de estas bocas es una charca hirviente de azufre, parecida al de Puracé, de furioso estrépito. Los vapores de azufre se escapan, además, de la tierra húmeda arcillosa y arrojan el lodo a lo alto, como si fuesen cañones." (Yudilevich Levy, 2004, p. 74).

With the assistance of Rüdiger Escobar-Wolf (Michigan Technological University), we translated the above passage as follows. Note that the works of von Humboldt were originally written in German.

"One of the depressions [of Azufral] contains a pond boiling and churning with sulfur, similar in appearance and furiously loud noises to the one at Puracé volcano. Sulfur vapors were also escaping from the clayey, humid earth, throwing the mud high in the air as if fired from cannons."

Local inhabitants shared their observations with von Humboldt, mentioning ash plumes (termed "polvo" in the diary), mud explosions, boiling water, and flames (sometimes starting brush fires) (Yudilevich Levy, 2004).

Explosive volcanic activity at Azufral had not been observed recently (a hydrothermal event was observed in July 2009, see the subsection below), but the geologic record has preserved evidence of large-scale eruptions dating from 2,095-950 BC (Siebert and others, 2010). In the January 2009 Technical Bulletin, the Servicio Geológico Colombiano (SGC) described Azufral as one of the most explosive volcanoes in Colombia due to its extensive pyroclastic and surge deposits.

Research by Hall and Mothes (2008) assessed Holocene volcanism and its impact on pre-Columbian indigenous cultures within the Interandean Valley. They synthesized the region's pyroclastic deposits (including source locations and event magnitudes) and highlighted the wide distribution of Azufral's deposits (figure 2). They argued that despite the extensive lahar and debris avalanche deposits within the valley, "the greatest impact upon mankind was probably not these short-lived violent events, but rather the burying of settlements and agricultural fields by ash fallout, the effect of which may have lasted hundreds of years. Ash fall layers are observed in pre-Columbian cultural horizons in the soil profile, occurring in the Interandean Valley, the lower flanks of the Andes, and along Ecuador's Pacific coast..."

Monitoring efforts 2005-2013. The base of operations for monitoring Azufral has been located in Pasto (~48 km ENE of Azufral) since ~2005. Over time, the Servicio Geológico Colombiano (SGC), formerly known as Instituto Colombiano de Geología y Minería (INGEOMINAS), expanded monitoring capabilities at Azufral through instrumentation and field investigations (table 1, figure 3).

Table 1. Azufral's monitoring network in March 2013 included EDM, seismometers, tiltmeters, a video camera, and a wind station. Figure 3, below, shows a map of various sites. Courtesy of SGC.

Station Description	Instrument Location(s)
Electronic Distance Meter (EDM) survey stations	12 reflectors; 4 base stations (see figure 14)
Seismic stations (telemetered)	Chaitán, ~4 km ENE (broadband); Laguna, 0.5 km SW (broadband); La Roca, 1.2 km E (short period)
Electronic tilt station (telemetered)	Chaitán, ~4 km ENE; La Roca, 1.2 km E
Web camera (telemetered)	Laguna, 0.5 km SW
Weather station (wind and precipitation)	La Roca, 1.2 km E

Aerial observations had been conducted since 2005 focusing primarily on the lake's characteristics such as color, water level, and shoreline morphology. Overflights with a thermal camera were conducted during 2007-2011; during that time period, the maximum surface temperatures ranged from 22.5-38°C.

Changes in the lake level were observed based on repeat aerial photos; in particular, between 5 December 2006 and 23 August 2009, Laguna Verde had a noticeably narrower shoreline, suggesting that the lake volume had increased.

Field investigations established baselines for lake chemistry, diffuse radon gas emissions, SO₂ flux within the crater, thermal emissions from fumarolic sites, EDM measurements, and the geochemistry of four local hot springs (figure 4).

During 2007-2008, SGC expanded the monitoring network by installing telemetered seismic stations and tiltmeters (figure 5). In the second quarter of 2008, the first monitoring stations were installed at Azufral; this timing coincided with monitoring developments at the neighboring volcanoes Doña Juana and Cumbal (volcanoes also managed by the Pasto Volcanological and Seismological Observatory, OVSP).

Seismicity 2009-2011. When Azufral's seismic stations came online in 2009, SGC began characterizing seismicity as volcano-tectonic (VT), long period (LPS), hybrid (HYB), tremor (TRE), tornillo (TOR), and unclassified (VOL). The VOL category, sometimes noted as "VC" in their reports, includes earthquakes from the region of Azufral that do not correspond with the other classes. SGC stated that these events will be analyzed in more detail after more baseline data is collected. This category was also applied to seismic analyses of Cumbal and Doña Juana, volcanos that were instrumented around the same time.

Unclassified seismicity (VOL) dominated the records through 2011, however, as SGC established baseline data, events falling in this category generally decreased over time. Total seismicity was also decreasing. During 2010-2011, tremor (TRE) and hybrid (HYB) events became sporadic to nonexistent.

During 5-6 February 2010, a seismic swarm was detected (figure 6). During January 2010-March 2013, this was the only swarm noted in the SGC Technical Bulletins. In early February 2010, two seismic stations were operating; Chaitán and La Roca. Unlike the Chaitán station, La Roca had broadband capabilities. "Broadband, high-dynamic-range seismometers are particularly important because existing instruments always saturate for large eruptions, and because energy at long periods (>>1 s) is simply not seen on standard short-period seismometers" (McNutt, 2000).

During April 2010, the highest number of earthquakes was detected (493 events); most of those events were VOL and LPS (table 2). Seismicity also increased in September (228 events); however, they were primarily VOL earthquakes.

Table 2. Azufral's seismicity from December 2009 to December 2011. No tornillo events were detected during this time period. For most of 2009, seismic station Chaitán was not fully functional. Abbreviations explained in text; "--" indicates intervals when the category was not included in the Technical Bulletins. Courtesy of SGC.

Month	VT	LPS	HYB	TRE	VOL	Total
Dec 2009	68	15	1	23	--	107
Jan 2010	2	3	0	3	0	8
Feb 2010	47	125	2	48	95	317
Mar 2010	20	25	0	18	80	143
Apr 2010	28	125	1	34	305	493
May 2010	23	45	0	14	97	179
Jun 2010	18	21	0	2	140	181
Jul 2010	36	29	0	15	119	199
Aug 2010	11	9	0	0	83	103
Sep 2010	12	6	0	--	210	228
Oct 2010	23	17	0	--	179	219
Nov 2010	21	11	0	--	72	104
Dec 2010	26	3	0	--	93	122
Jan 2011	32	21	0	--	93	146
Feb 2011	30	2	0	--	109	141
Mar 2011	14	23	0	--	68	105
Apr 2011	29	20	0	--	86	135
May 2011	11	1	0	--	40	52
Jun 2011	18	9	1	--	30	58
Jul 2011	20	3	0	--	21	44
Aug 2011	4	0	0	--	10	14
Sep 2011	4	1	0	--	14	19
Oct 2011	8	2	1	--	12	23
Nov 2011	12	7	3	--	33	55
Dec 2011	13	--	--	--	22	35

Overall 2011 seismicity averaged ~69 events per day (table 2). Earthquakes occurred more frequently earlier in the year; during January-May they averaged 116 events per month compared with 35 per month during June-December.

On 20 July 2011 at 0353, an earthquake was felt by local populations, particularly in the town of El Panamal (~5 km SW). The event was an M_L 3 at 12.8 km depth (measured relative to the summit) and epicenter at 9.5 km SW. This was the only located earthquake that month; at that time, two seismic stations were operating (Chaitán and La Roca).

Seismicity in 2012-2013. In 2012, 5-45 VT earthquakes were recorded per month and 1-19 were located (table 3). At 19:41 on 4 May 2012, an earthquake was felt by local populations in Túquerres, San Roque, and Sapuyes (for town locations, see figure 3). It was an M_L 3.3 with an epicenter ~12.2 km of Azufral at a depth of 8.64 km. The maximum intensity of shaking was III on the Modified Mercalli scale.

Table 3. Seismicity at Azufral from January 2012 through April 2013. Note that depths of events are measured relative to the established summit elevation (4,070 m elevation). Courtesy of SGC.

Month	VT	VT Located	VT ML	VT Depths	VT Epicenter	VOL	Total
Jan 2012	19	--	--	--	--	15	34
Feb 2012	45	--	--	--	--	20	65
Mar 2012	10	--	--	--	--	5	15
Apr 2012	20	--	--	--	--	3	23
May 2012	14	2	3.3; 1.7	8.6 km; 7.4 km	12.2 km E; 6 km NW	1	15
Jun 2012	6	--	--	--	--	1	7
Jul 2012	5	1	1.4	15 km	3.4 km NE	2	7
Aug 2012	7	--	--	--	--	0	7
Sep 2012	9	2	2.1; 2.9	~6 km; ~14 km	10 km SE; 14 km E	0	9
Oct 2012	42	19	0.5-2.1	< 16 km	1.5-15 km E	8	50
Nov 2012	22	2	0.6-0.7	< 2 km	4 km NE; 11 km NE	5	27
Dec 2012	24	1	0.8	16 km	10.4 km NE	50	74
Jan 2013	15	1	1.1	4.7 km	2.5 km N	9	24
Feb 2013	15	6	0.3-1.9	2.5-15 km	< 1-< 11 km	6	21
Mar 2013	16	2	< 1.3	5.4 km; 7.3 km	7 km S; 3.5 km N	0	16
Apr 2013	39	26	< 2.1	< 11 km	4-10 km dispersed	15	54

During 2012, the largest number of located earthquakes occurred in October 2012. Located earthquakes peaked later in April 2013. Of the 39 VT detected, 26 of these earthquakes were located, primarily in a scattered cluster ~8 km NW of the summit (figure 7).

Field observations in 2008 and mid-2009. During geophysical campaigns carried out in 2008 by SGC (then INGEOMINAS), fumarolic activity was observed from one of its domes, Domo Pequeño, in an area lacking vegetation. That location was also known for sulfur deposits, causing the surface to appear greenish-yellow; sulfur odors could were also detected. Bubbles in Laguna Verde were also apparent, rising from deep in Laguna Verde.

Aerial photos taken on 13 April 2009 showed clear views of the pale dome rock and bright green lake. A visit on 23 June 2009, revealed a zone of cloudy water in the green lake; low-level fumarolic activity was also observed (figure 8).

Hydrothermal explosion in July 2009. SGC technicians had visited Azufral on 12 July 2009 to take water samples for analysis, but a group of scientists visiting on 18 July were surprised by a sudden change within the crater. They discovered a new deposit, 8-10 m long extending from the fumarolic region known as La Playa; the deposits were described as hot and they had extended into the lake. The SGC surmised that the activity must have occurred between the 13 and 18 July 2009. The group determined that this was an eruptive process likely of hydrothermal origin. The visiting scientists (from Fundación Ambiental Andes) reported observations including fresh-looking cracks and several slope failures which had allowed hot fluids to escape; those areas continued to steam during their visit (figure 9).

In looking for monitoring signals during 13-18 July, SGC found that seismic and tilt data lacked clear elevated activity in July 2009; there were few earthquakes and mainly minor changes detected by the tilt instruments at Chaitán). Looking in more detail, the tilt station recorded some variations during 12-23 July, particularly from the X component (radial to the crater lake) (figure 10). A total decrease of 45 µrad was recorded while the Y component (tangential to the crater lake) was relatively stable with a slight increase of ~10 µrad and temperatures were between 6.5 and 9°C.

August 2009 field investigations. On 3 August, a local observer noted unusual activity while walking along the higher peaks of Azufral; he stated that he saw "material being set on fire in the beach of Azufral and there were gases smelling like sulfur." A local landowner also explained that hot springs could be found ~6.5 km away at a site called Tutachag; these springs had persisted for several months. SGC alerted the local disaster prevention representative (Comité Regional de Prevención y Atención de Desastres de Nariño, CREPAD-N) after receiving the report of these observations; the CREPAD-N is responsible for communicating with local residents and visitors who frequent sites around Azufral.

During field investigations on 18 August, SGC staff learned from an additional local inhabitant (from the town of San Roque Alto) that, while walking the road to La Palma early in the morning of 3 August, he thought there was a fire on La Playa, possibly started by tourists. The fire was blue and red (although mostly blue) and gray smoke was rising, sometimes dense gray; he also noted sulfur odors.

After reviewing the seismicity during the first week of August 2009, SGC staff noted small events had been detected by the Chaitán station. At that time, seismic monitoring was not robust enough to provide earthquake locations, but the records determined that low pulses of spasmodic tremor had occurred in the range of 6-12 Hz and 12-18 Hz, lasting up to 4 minutes. LP events were also apparent in the record.

On 19 August, visiting scientists noted increased bubbling from more locations within Laguna Verde; primarily around the N shore of the lake. Few emissions were observed from the La Playa area; however, they noted intermittent sulfur odors while they conducted fieldwork.

SGC scientists traversed the NE shoreline with a FLIR (Forward Looking Infrared) thermal camera. The temperatures reached a maximum of 57.9°C along the N shore of La Playa (figure 11). Maximum temperatures corresponded with known locations of past hydrothermal activity.

On 19 August, SGC scientists measured SO₂ emissions along a traverse with Mobile DOAS. The team followed ~50 m of the shore and calculated an average flux of 0.5 tons per day, a value considered relatively low. They noted that the wind was from the N at 2.5 m/s.

Samples of the deposits attributed to the 13-18 July event on La Playa were distinctively cemented and possibly rich in silica and alteration minerals (figure 12). The SGC scientists collected samples for lab analysis including x-ray diffraction (XRD). Two samples were analyzed at SGC laboratory in Cali where XRD determined abundant (>40%) sulfur was present; amorphous silica (opal) was sparse (3-10%) and trace quantities (

On 30 August an experiment was conducted with small fragments of this material. In a lab setting, SGC scientists demonstrated that the material was flammable and produced heat and sulfur odors that stung the eyes and nose; red and blue flames were also observed immediately when the fragments encountered an open flame (tested with a lighted match). After a few seconds of exposure to an open flame, the samples melted and immediately crumbled into an inert, brittle solid. This demonstration may explain the explosive phenomena that local inhabitants observed on 3 August 2009.

Aerial observations during August-December 2009. During 11 and 19 September, the FAC facilitated observations of Azufral. Photographs and thermal imagery revealed few changes. The highest temperatures detected were in range of 25 to 30°C. The largest region of thermal anomalies was located on the opposite shore from La Playa (figure 13), a region where dacitic domes have been known to emit steam and have sulfur deposits.

A return trip to Azufral during 7-11 December 2009 determined that some emissions were visibly rising from the dome located on the E side of Laguna Verde (figure 14). A maximum temperature measured from the dome was 85°C. SGC scientists also measured concentrations of CO₂ higher than 10,000 ppm from fumarolic sites.

Emission sites were also revisited along La Playa on 9 December. Temperatures measured with a thermocouple were in the range of 65-84°C. Those temperatures were measured at locations that had elevated temperatures when last measured with a FLIR. CO₂ emissions from these zones reached 3,200 ppm.

2010-2012 monitoring highlights. Routine monitoring from January 2010 to 2012 included sampling Laguna Verde at several locations as well as sampling the local hotsprings (figure 4). By October 2010, a baseline of geochemical data was developed by SGC and the four distal hot springs were evaluated and characterized as primarily mature-to-peripheral water (figure 15).

Monitoring temperatures from Laguna Verde and selected sites also continued during 2010-2012. SGC scientists frequently conducted traverses along the shore with a thermocouple and established baseline temperature data (figure 16).

During field campaigns, SCG staff noted variable emissions from fumarolic sites, clustering of bubbles within Laguna Verde, and also changes in the lake level. To aid visual monitoring, a web camera was installed within the crater of Azufral on 24 November 2012 (figure 17). The camera was positioned to include a wide view of Domo Pequeño (a regular source of steam emissions) and La Playa (the location of the hydrothermal event in July 2009).

References. Hall, M.L and Mothes, P.A., 2008. Volcanic impediments in the progressive development of pre-Columbian civilizations in the Ecuadorian Andes, Journal of Volcanology and Geothermal Research, 176, 344-355.

McNutt, S.R., 2000, Volcanic seismicity. In: Sigurdsson, H., ed., Encyclopedia of volcanoes. New York, Academic Press, p. 1,015-1,033.

Siebert, L., Simkin, T., Kimberly, P., 2010, Volcanoes of the World, 3rd edn. University of California Press, Berkeley.

Yudilevich Levy, D., 2004, Mi viaje por el camino del Inca (1801-1802): Antología, 1a. ed., Editorial Universitaria, S.A., Santiago, Chile [in Spanish].

Information Contacts: Servicio Geológico Colombiano (SGC), Observatorio Vulcanológico y Sismológico de Pasto, Pasto, Colombia (URL: http://www.SGC.gov.co/Pasto.aspx); Patricia Ponce Villarreal, Servicio Geológico Colombiano (SGC), Observatorio Vulcanológico y Sismológico de Pasto, Pasto, Colombia (URL: http://www.SGC.gov.co/Pasto.aspx); Rüdiger Escobar-Wolf, Michigan Technological University, Department of Geological and Mining Engineering and Science, Houghton, MI, USA (URL: http://www.mtu.edu/geo/).

Information is preliminary and subject to change. All times are local (unless otherwise noted)

May 1971 (CSLP 43-71)

More than 60 tremors felt since 26 April

Card 1197 (07 May 1971) More than 60 tremors felt since 26 April

The following was received on 7 May 1971. "More than 60 local tremors near Azufral have been felt by inhabitants of the village Santander, Nariño, Colombia, starting 26 April. Some have been registered (none felt) at Pasto Seismic Station, 215 km away. The origin of this swarm of tremors seems to be underground movement of volcanic origin without outside of any volcanic activity."

Information Contacts: S.J. Jesus Ramirez, Instituto Geofísico de los Andes, Bogota, Colombia.

August 1990 (BGVN 15:08) Cite this Report

Fumaroles near young summit domes; extra-caldera ignimbrites may be only hundreds of years old

"Azufral caldera, with associated dome complex, was visited during July and August 1990. The major goal of current research, by the Univ de Montréal, is to map the stratigraphy of the caldera-filling dome sequence and the very young ignimbrites, distributed primarily S and E of the complex. Within the summit caldera, a lake (Laguna Verde) had a temperature of 8°C and pH of 2.4. The lake was a distinct clear emerald green, notably not the opaque milky green of an extremely acid lake such as at Poás, Costa Rica. The hottest springs found on the NE edge of the lake had a temperature of 54°C and pH of 2.6. More acid vents must be located beneath the lake to produce its low pH. Giggenbach-type samples were collected from the lake-edge bubbles. The highest fumarole temperatures, encountered on the youngest rhyodacite dome, were 87°C. Extensive alteration was evident, usually near the base of the domes. Bedded tuffs and tuff breccias, on the NE side of the lake, appeared to be related to hydrothermal explosions. The relative stratigraphy of the domes was indicated by their youthful morphology, with those on the E side appearing to be the youngest. A series of wave-cut terraces around the lake extended to 4-5 m above the present lake level. Between early July and August, lake level dropped by ~ 5 cm, probably in response to the dry season that normally begins in July. Outside the caldera the rhyodacite ignimbrites appeared, from stratigraphy and erosion, to be young - perhaps less than several hundred years. Fumarolic activity at Azufral does not appear to be significantly influenced by volcanic processes."

Information Contacts: S. Williams, Louisiana State Univ; J. Stix and E. Fontaine, Univ de Montréal.

March 2013 (BGVN 38:03) Cite this Report

Expanded monitoring efforts and explosive hydrothermal event in July 2009

Previously reported activity from Azufral included seismic swarms in 1971 (CSLP 43-71) and fluctuating conditions within the crater lake, Laguna Verde during July-August 1990 (BGVN 15:08) (figure 1). In this report, we highlight explosive hydrothermal activity that occurred during July-August 2009. We also provide observations of Azufral's hydrothermal and fumarolic activity and review monitoring efforts that expanded since 2005.

Fumarolic activity within Azufral's largest crater had long been observed by Colombia's earliest inhabitants and investigators including Alexander von Humboldt in the 1800s (Yudilevich Levy, 2004). In one of his many journals, Diario VII "Viaje de Pasto a Quito," this naturalist noted the rugged morphology of the edifice, describing it as a volcano that had broken apart; similar in appearance to Sotará, a volcano he had already visited. At the time of his visit in December 1801, there were significant deposits of sulfur and strong gas emissions within the crater, particularly around the largest crater lake (he noted that there were several craters in the complex, the largest now known as Laguna Verde).

"Una de estas bocas es una charca hirviente de azufre, parecida al de Puracé, de furioso estrépito. Los vapores de azufre se escapan, además, de la tierra húmeda arcillosa y arrojan el lodo a lo alto, como si fuesen cañones." (Yudilevich Levy, 2004, p. 74).

With the assistance of Rüdiger Escobar-Wolf (Michigan Technological University), we translated the above passage as follows. Note that the works of von Humboldt were originally written in German.

"One of the depressions [of Azufral] contains a pond boiling and churning with sulfur, similar in appearance and furiously loud noises to the one at Puracé volcano. Sulfur vapors were also escaping from the clayey, humid earth, throwing the mud high in the air as if fired from cannons."

Local inhabitants shared their observations with von Humboldt, mentioning ash plumes (termed "polvo" in the diary), mud explosions, boiling water, and flames (sometimes starting brush fires) (Yudilevich Levy, 2004).

Explosive volcanic activity at Azufral had not been observed recently (a hydrothermal event was observed in July 2009, see the subsection below), but the geologic record has preserved evidence of large-scale eruptions dating from 2,095-950 BC (Siebert and others, 2010). In the January 2009 Technical Bulletin, the Servicio Geológico Colombiano (SGC) described Azufral as one of the most explosive volcanoes in Colombia due to its extensive pyroclastic and surge deposits.

Research by Hall and Mothes (2008) assessed Holocene volcanism and its impact on pre-Columbian indigenous cultures within the Interandean Valley. They synthesized the region's pyroclastic deposits (including source locations and event magnitudes) and highlighted the wide distribution of Azufral's deposits (figure 2). They argued that despite the extensive lahar and debris avalanche deposits within the valley, "the greatest impact upon mankind was probably not these short-lived violent events, but rather the burying of settlements and agricultural fields by ash fallout, the effect of which may have lasted hundreds of years. Ash fall layers are observed in pre-Columbian cultural horizons in the soil profile, occurring in the Interandean Valley, the lower flanks of the Andes, and along Ecuador's Pacific coast..."

Monitoring efforts 2005-2013. The base of operations for monitoring Azufral has been located in Pasto (~48 km ENE of Azufral) since ~2005. Over time, the Servicio Geológico Colombiano (SGC), formerly known as Instituto Colombiano de Geología y Minería (INGEOMINAS), expanded monitoring capabilities at Azufral through instrumentation and field investigations (table 1, figure 3).

Table 1. Azufral's monitoring network in March 2013 included EDM, seismometers, tiltmeters, a video camera, and a wind station. Figure 3, below, shows a map of various sites. Courtesy of SGC.

Station Description	Instrument Location(s)
Electronic Distance Meter (EDM) survey stations	12 reflectors; 4 base stations (see figure 14)
Seismic stations (telemetered)	Chaitán, ~4 km ENE (broadband); Laguna, 0.5 km SW (broadband); La Roca, 1.2 km E (short period)
Electronic tilt station (telemetered)	Chaitán, ~4 km ENE; La Roca, 1.2 km E
Web camera (telemetered)	Laguna, 0.5 km SW
Weather station (wind and precipitation)	La Roca, 1.2 km E

Aerial observations had been conducted since 2005 focusing primarily on the lake's characteristics such as color, water level, and shoreline morphology. Overflights with a thermal camera were conducted during 2007-2011; during that time period, the maximum surface temperatures ranged from 22.5-38°C.

Changes in the lake level were observed based on repeat aerial photos; in particular, between 5 December 2006 and 23 August 2009, Laguna Verde had a noticeably narrower shoreline, suggesting that the lake volume had increased.

Field investigations established baselines for lake chemistry, diffuse radon gas emissions, SO₂ flux within the crater, thermal emissions from fumarolic sites, EDM measurements, and the geochemistry of four local hot springs (figure 4).

During 2007-2008, SGC expanded the monitoring network by installing telemetered seismic stations and tiltmeters (figure 5). In the second quarter of 2008, the first monitoring stations were installed at Azufral; this timing coincided with monitoring developments at the neighboring volcanoes Doña Juana and Cumbal (volcanoes also managed by the Pasto Volcanological and Seismological Observatory, OVSP).

Seismicity 2009-2011. When Azufral's seismic stations came online in 2009, SGC began characterizing seismicity as volcano-tectonic (VT), long period (LPS), hybrid (HYB), tremor (TRE), tornillo (TOR), and unclassified (VOL). The VOL category, sometimes noted as "VC" in their reports, includes earthquakes from the region of Azufral that do not correspond with the other classes. SGC stated that these events will be analyzed in more detail after more baseline data is collected. This category was also applied to seismic analyses of Cumbal and Doña Juana, volcanos that were instrumented around the same time.

Unclassified seismicity (VOL) dominated the records through 2011, however, as SGC established baseline data, events falling in this category generally decreased over time. Total seismicity was also decreasing. During 2010-2011, tremor (TRE) and hybrid (HYB) events became sporadic to nonexistent.

During 5-6 February 2010, a seismic swarm was detected (figure 6). During January 2010-March 2013, this was the only swarm noted in the SGC Technical Bulletins. In early February 2010, two seismic stations were operating; Chaitán and La Roca. Unlike the Chaitán station, La Roca had broadband capabilities. "Broadband, high-dynamic-range seismometers are particularly important because existing instruments always saturate for large eruptions, and because energy at long periods (>>1 s) is simply not seen on standard short-period seismometers" (McNutt, 2000).

During April 2010, the highest number of earthquakes was detected (493 events); most of those events were VOL and LPS (table 2). Seismicity also increased in September (228 events); however, they were primarily VOL earthquakes.

Table 2. Azufral's seismicity from December 2009 to December 2011. No tornillo events were detected during this time period. For most of 2009, seismic station Chaitán was not fully functional. Abbreviations explained in text; "--" indicates intervals when the category was not included in the Technical Bulletins. Courtesy of SGC.

Month	VT	LPS	HYB	TRE	VOL	Total
Dec 2009	68	15	1	23	--	107
Jan 2010	2	3	0	3	0	8
Feb 2010	47	125	2	48	95	317
Mar 2010	20	25	0	18	80	143
Apr 2010	28	125	1	34	305	493
May 2010	23	45	0	14	97	179
Jun 2010	18	21	0	2	140	181
Jul 2010	36	29	0	15	119	199
Aug 2010	11	9	0	0	83	103
Sep 2010	12	6	0	--	210	228
Oct 2010	23	17	0	--	179	219
Nov 2010	21	11	0	--	72	104
Dec 2010	26	3	0	--	93	122
Jan 2011	32	21	0	--	93	146
Feb 2011	30	2	0	--	109	141
Mar 2011	14	23	0	--	68	105
Apr 2011	29	20	0	--	86	135
May 2011	11	1	0	--	40	52
Jun 2011	18	9	1	--	30	58
Jul 2011	20	3	0	--	21	44
Aug 2011	4	0	0	--	10	14
Sep 2011	4	1	0	--	14	19
Oct 2011	8	2	1	--	12	23
Nov 2011	12	7	3	--	33	55
Dec 2011	13	--	--	--	22	35

Overall 2011 seismicity averaged ~69 events per day (table 2). Earthquakes occurred more frequently earlier in the year; during January-May they averaged 116 events per month compared with 35 per month during June-December.

On 20 July 2011 at 0353, an earthquake was felt by local populations, particularly in the town of El Panamal (~5 km SW). The event was an M_L 3 at 12.8 km depth (measured relative to the summit) and epicenter at 9.5 km SW. This was the only located earthquake that month; at that time, two seismic stations were operating (Chaitán and La Roca).

Seismicity in 2012-2013. In 2012, 5-45 VT earthquakes were recorded per month and 1-19 were located (table 3). At 19:41 on 4 May 2012, an earthquake was felt by local populations in Túquerres, San Roque, and Sapuyes (for town locations, see figure 3). It was an M_L 3.3 with an epicenter ~12.2 km of Azufral at a depth of 8.64 km. The maximum intensity of shaking was III on the Modified Mercalli scale.

Table 3. Seismicity at Azufral from January 2012 through April 2013. Note that depths of events are measured relative to the established summit elevation (4,070 m elevation). Courtesy of SGC.

Month	VT	VT Located	VT ML	VT Depths	VT Epicenter	VOL	Total
Jan 2012	19	--	--	--	--	15	34
Feb 2012	45	--	--	--	--	20	65
Mar 2012	10	--	--	--	--	5	15
Apr 2012	20	--	--	--	--	3	23
May 2012	14	2	3.3; 1.7	8.6 km; 7.4 km	12.2 km E; 6 km NW	1	15
Jun 2012	6	--	--	--	--	1	7
Jul 2012	5	1	1.4	15 km	3.4 km NE	2	7
Aug 2012	7	--	--	--	--	0	7
Sep 2012	9	2	2.1; 2.9	~6 km; ~14 km	10 km SE; 14 km E	0	9
Oct 2012	42	19	0.5-2.1	< 16 km	1.5-15 km E	8	50
Nov 2012	22	2	0.6-0.7	< 2 km	4 km NE; 11 km NE	5	27
Dec 2012	24	1	0.8	16 km	10.4 km NE	50	74
Jan 2013	15	1	1.1	4.7 km	2.5 km N	9	24
Feb 2013	15	6	0.3-1.9	2.5-15 km	< 1-< 11 km	6	21
Mar 2013	16	2	< 1.3	5.4 km; 7.3 km	7 km S; 3.5 km N	0	16
Apr 2013	39	26	< 2.1	< 11 km	4-10 km dispersed	15	54

During 2012, the largest number of located earthquakes occurred in October 2012. Located earthquakes peaked later in April 2013. Of the 39 VT detected, 26 of these earthquakes were located, primarily in a scattered cluster ~8 km NW of the summit (figure 7).

Field observations in 2008 and mid-2009. During geophysical campaigns carried out in 2008 by SGC (then INGEOMINAS), fumarolic activity was observed from one of its domes, Domo Pequeño, in an area lacking vegetation. That location was also known for sulfur deposits, causing the surface to appear greenish-yellow; sulfur odors could were also detected. Bubbles in Laguna Verde were also apparent, rising from deep in Laguna Verde.

Aerial photos taken on 13 April 2009 showed clear views of the pale dome rock and bright green lake. A visit on 23 June 2009, revealed a zone of cloudy water in the green lake; low-level fumarolic activity was also observed (figure 8).

Hydrothermal explosion in July 2009. SGC technicians had visited Azufral on 12 July 2009 to take water samples for analysis, but a group of scientists visiting on 18 July were surprised by a sudden change within the crater. They discovered a new deposit, 8-10 m long extending from the fumarolic region known as La Playa; the deposits were described as hot and they had extended into the lake. The SGC surmised that the activity must have occurred between the 13 and 18 July 2009. The group determined that this was an eruptive process likely of hydrothermal origin. The visiting scientists (from Fundación Ambiental Andes) reported observations including fresh-looking cracks and several slope failures which had allowed hot fluids to escape; those areas continued to steam during their visit (figure 9).

In looking for monitoring signals during 13-18 July, SGC found that seismic and tilt data lacked clear elevated activity in July 2009; there were few earthquakes and mainly minor changes detected by the tilt instruments at Chaitán). Looking in more detail, the tilt station recorded some variations during 12-23 July, particularly from the X component (radial to the crater lake) (figure 10). A total decrease of 45 µrad was recorded while the Y component (tangential to the crater lake) was relatively stable with a slight increase of ~10 µrad and temperatures were between 6.5 and 9°C.

August 2009 field investigations. On 3 August, a local observer noted unusual activity while walking along the higher peaks of Azufral; he stated that he saw "material being set on fire in the beach of Azufral and there were gases smelling like sulfur." A local landowner also explained that hot springs could be found ~6.5 km away at a site called Tutachag; these springs had persisted for several months. SGC alerted the local disaster prevention representative (Comité Regional de Prevención y Atención de Desastres de Nariño, CREPAD-N) after receiving the report of these observations; the CREPAD-N is responsible for communicating with local residents and visitors who frequent sites around Azufral.

During field investigations on 18 August, SGC staff learned from an additional local inhabitant (from the town of San Roque Alto) that, while walking the road to La Palma early in the morning of 3 August, he thought there was a fire on La Playa, possibly started by tourists. The fire was blue and red (although mostly blue) and gray smoke was rising, sometimes dense gray; he also noted sulfur odors.

After reviewing the seismicity during the first week of August 2009, SGC staff noted small events had been detected by the Chaitán station. At that time, seismic monitoring was not robust enough to provide earthquake locations, but the records determined that low pulses of spasmodic tremor had occurred in the range of 6-12 Hz and 12-18 Hz, lasting up to 4 minutes. LP events were also apparent in the record.

On 19 August, visiting scientists noted increased bubbling from more locations within Laguna Verde; primarily around the N shore of the lake. Few emissions were observed from the La Playa area; however, they noted intermittent sulfur odors while they conducted fieldwork.

SGC scientists traversed the NE shoreline with a FLIR (Forward Looking Infrared) thermal camera. The temperatures reached a maximum of 57.9°C along the N shore of La Playa (figure 11). Maximum temperatures corresponded with known locations of past hydrothermal activity.

On 19 August, SGC scientists measured SO₂ emissions along a traverse with Mobile DOAS. The team followed ~50 m of the shore and calculated an average flux of 0.5 tons per day, a value considered relatively low. They noted that the wind was from the N at 2.5 m/s.

Samples of the deposits attributed to the 13-18 July event on La Playa were distinctively cemented and possibly rich in silica and alteration minerals (figure 12). The SGC scientists collected samples for lab analysis including x-ray diffraction (XRD). Two samples were analyzed at SGC laboratory in Cali where XRD determined abundant (>40%) sulfur was present; amorphous silica (opal) was sparse (3-10%) and trace quantities (

On 30 August an experiment was conducted with small fragments of this material. In a lab setting, SGC scientists demonstrated that the material was flammable and produced heat and sulfur odors that stung the eyes and nose; red and blue flames were also observed immediately when the fragments encountered an open flame (tested with a lighted match). After a few seconds of exposure to an open flame, the samples melted and immediately crumbled into an inert, brittle solid. This demonstration may explain the explosive phenomena that local inhabitants observed on 3 August 2009.

Aerial observations during August-December 2009. During 11 and 19 September, the FAC facilitated observations of Azufral. Photographs and thermal imagery revealed few changes. The highest temperatures detected were in range of 25 to 30°C. The largest region of thermal anomalies was located on the opposite shore from La Playa (figure 13), a region where dacitic domes have been known to emit steam and have sulfur deposits.

A return trip to Azufral during 7-11 December 2009 determined that some emissions were visibly rising from the dome located on the E side of Laguna Verde (figure 14). A maximum temperature measured from the dome was 85°C. SGC scientists also measured concentrations of CO₂ higher than 10,000 ppm from fumarolic sites.

Emission sites were also revisited along La Playa on 9 December. Temperatures measured with a thermocouple were in the range of 65-84°C. Those temperatures were measured at locations that had elevated temperatures when last measured with a FLIR. CO₂ emissions from these zones reached 3,200 ppm.

2010-2012 monitoring highlights. Routine monitoring from January 2010 to 2012 included sampling Laguna Verde at several locations as well as sampling the local hotsprings (figure 4). By October 2010, a baseline of geochemical data was developed by SGC and the four distal hot springs were evaluated and characterized as primarily mature-to-peripheral water (figure 15).

Monitoring temperatures from Laguna Verde and selected sites also continued during 2010-2012. SGC scientists frequently conducted traverses along the shore with a thermocouple and established baseline temperature data (figure 16).

During field campaigns, SCG staff noted variable emissions from fumarolic sites, clustering of bubbles within Laguna Verde, and also changes in the lake level. To aid visual monitoring, a web camera was installed within the crater of Azufral on 24 November 2012 (figure 17). The camera was positioned to include a wide view of Domo Pequeño (a regular source of steam emissions) and La Playa (the location of the hydrothermal event in July 2009).

References. Hall, M.L and Mothes, P.A., 2008. Volcanic impediments in the progressive development of pre-Columbian civilizations in the Ecuadorian Andes, Journal of Volcanology and Geothermal Research, 176, 344-355.

McNutt, S.R., 2000, Volcanic seismicity. In: Sigurdsson, H., ed., Encyclopedia of volcanoes. New York, Academic Press, p. 1,015-1,033.

Siebert, L., Simkin, T., Kimberly, P., 2010, Volcanoes of the World, 3rd edn. University of California Press, Berkeley.

Yudilevich Levy, D., 2004, Mi viaje por el camino del Inca (1801-1802): Antología, 1a. ed., Editorial Universitaria, S.A., Santiago, Chile [in Spanish].

Information Contacts: Servicio Geológico Colombiano (SGC), Observatorio Vulcanológico y Sismológico de Pasto, Pasto, Colombia (URL: http://www.SGC.gov.co/Pasto.aspx); Patricia Ponce Villarreal, Servicio Geológico Colombiano (SGC), Observatorio Vulcanológico y Sismológico de Pasto, Pasto, Colombia (URL: http://www.SGC.gov.co/Pasto.aspx); Rüdiger Escobar-Wolf, Michigan Technological University, Department of Geological and Mining Engineering and Science, Houghton, MI, USA (URL: http://www.mtu.edu/geo/).