Soufriere Guadeloupe

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  • 16.044°N
  • 61.664°W

  • 1467 m
    4812 ft

  • 360060
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Most Recent Bulletin Report: March 1983 (SEAN 08:03)


Water temperatures and chemistry

A study of the geochemical evolution of Carbet l'Echelle spring, continued during 1981 and 1982 (figure 10). The water temperature decreased from 62.5°C in January 1981 to 50° in September 1982, while the concentration of HCO3 ions continued to increase (+ 30%). Moreover, although large variations in Cl concentration have been observed since 1979, the background level of Cl began to fall in September 1981 and was reduced by half in one year. Likewise, the concentration of F ions, which has oscillated around a constant value since the beginning of the survey, decreased slightly in late 1982. Water temperatures and chemistry remained nearly constant at the other springs monitored by this study.

Figure 10. Changes in temperature (°C), HCO3 and Cl concentration (103 moles/liter), and F concentration (105 moles/liter) for Carbet l'Echelle spring, 500 m from the summit of Soufrière Guadeloupe, January 1981-September 1982.

Further References: Bigot, S., and Hammouya, G., 1987, Surveillance hydrogéochimique de la Soufrière de Guadeloupe, 1979-1985: Diminuition d'activité ou confinement?: C.R. Acad. Sci. Paris, t. 304, Série II, no. 13, p. 757-760.

Observations volcanologiques: Rapport d'Activite des Observatoires Volcanologiques des Antilles (Guadeloupe-Martinique) - November 1976-April 1977, April 1977-December 1978, 1979, 1980, 1981, 1982, and 1983-1984: Institut de Physique du Globe, Paris.

Information Contacts: S. Bigot, Lab. de Géochemie, Paris; G. Hammouya, Lab. de Physique du Globe; J. Le Mouel, J. Cheminée, IPG, Paris.

The Global Volcanism Program has no Weekly Reports available for Soufriere Guadeloupe.

Index of Bulletin Reports


Reports are organized chronologically and indexed below by Month/Year (Publication Volume:Number), and include a one-line summary. Click on the index link or scroll down to read the reports.

04/1976 (NSEB 01:07) Seismic crisis during November 1975-April 1976; no surface activity

06/1976 (NSEB 01:09) Phreatic eruption on 8 July; crack opens in summit dome

07/1976 (NSEB 01:10) Additional details about 8 July phreatic explosion; summary of activity during 21 July-25 August 1976

08/1976 (NSEB 01:11) Summary of activity during 2-15 September 1976

09/1976 (NSEB 01:12) Variable activity continues; ash eruption on 22 September

10/1976 (NSEB 01:13) Eruption on 2 October deposits ash 7 km away; continued steam emission

11/1976 (NSEB 01:14) Phreatic explosions and mild steaming; evacuation ends 1 December

12/1976 (NSEB 01:15) Mild steaming with an occasional weak phreatic explosion

01/1977 (NSEB 02:01) Summary of steam-and-ash explosions during October 1976-January 1977

02/1977 (NSEB 02:02) Phreatic activity continues; large explosion on 29 January

03/1977 (NSEB 02:03) Earthquake rate decreases to 1 per day

04/1977 (NSEB 02:04) Decreased seismic and surface activity

05/1977 (NSEB 02:05) Fumarolic activity

06/1977 (NSEB 02:06) Summary of seismicity since mid-1975

10/1981 (SEAN 06:10) Temperature, magnetic field stable

01/1982 (SEAN 07:01) Temperatures and chemistry of thermal springs

03/1983 (SEAN 08:03) Water temperatures and chemistry




Bulletin Reports

All information contained in these reports is preliminary and subject to change.


04/1976 (NSEB 01:07) Seismic crisis during November 1975-April 1976; no surface activity

The recent seismic crisis began in November 1975 when 25 tremors were recorded. Thirty tremors were registered in December, 36 in January 1976, 93 in February, and 680 in March (of which 1/3 were felt by inhabitants very near the volcano). The crisis was declining at the end of April. The foci of the tremors were under the NW part of Soufrière, and depths of focus varied from 1 to 5 km.

No new surface manifestations accompanied or followed these tremors (up to 9 April). There were no modifications of temperatures nor of the composition of gases emitted by the fumaroles. An overflight of the volcano did not indicate any sign of abnormal activity on the surface. . . .

Local earthquake swarms are rather frequent at volcanoes of this type. They have taken place approximately once per year on Guadeloupe since 1962, but none have reached the frequency of March 1976. The same phenomenon has previously occurred on neighboring islands (Montserrat 1966, St. Kitts in 1950 and 1961, and St. Vincent 1947) without any eruption.

J. Dorel believes that, for the present time, there is no important risk of an eruption of this volcano, but that it is impossible to make a long-term (several months or years) prognostication on the evolution of such volcanoes.

Information Contacts: J. Dorel, IPG, Paris.
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06/1976 (NSEB 01:09) Phreatic eruption on 8 July; crack opens in summit dome

On 8 July at approximately 0900, a phreatic eruption began at Soufrière (figure 1). A new crack, 300 m long [but see 1:10] and up to 10 m wide, opened down the SE side of the summit dome. Steam and gas with ash and lava fragments were blowing through the crack on that day, but on 9 July there were only steam and gas with no solids. The eruption appeared to be purely phreatic, with no molten material reported.

Figure 1. Map of the S part of Basse-Terre (one of the islands that comprise Guadeloupe). After Guadeloupe Tourist Map, 1:100,000, Institut Géographique National, 1982.

On the 9th the gas and steam were venting at a "vast rate," and the column rose ~300 m above the crack. Steam and gas venting was continuing as of this report, but the activity appeared to be slowing down. It was not possible to ascertain the height of the steam column because of clouds. It is believed that local earthquakess occurred just before the eruptive activity began; longer-term premonitory seismicity was described in 1:8.

A phreatic eruption occurred in 1956 from a fracture across the top of the dome (figure 2), but the current eruption is bigger in that the crack is longer and the volume of products is greater. There were comparable phreatic eruptions in [1837-38] and 1797, each lasting a few days. The present activity appears to be following the pattern of these previous eruptions. Radiocarbon evidence indicates that there was a large magmatic eruption about 1500 A.D.

Figure 2. Map of the summit of Soufrière volcano, Guadeloupe, after Catalog of Active Volcanoes of the World. Heights are in meters.

In general characteristics Soufrière is comparable to the Martinique and St. Vincent volcanoes, which are capable of extremely violent activity.

Information Contacts: J. Tomblin, UWI; Lab. de Physique du Globe.
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07/1976 (NSEB 01:10) Additional details about 8 July phreatic explosion; summary of activity during 21 July-25 August 1976

Since March 1976 a great number of volcanic earthquakes have been registered by the seismic array of the Observatory of St. Claude, Guadeloupe. The earthquakes numbered about 607 in March, 747 in April, 611 in May, and 668 in June. Most foci were distributed between 2 and 6 km under the volcano, along a NW-SE axis. Many earthquakes were felt by people living near Soufrière. The maximum magnitude was 3.8.

On 8 July at 0856, the volcano threw out a column of fine sand and dust, plunging the surrounding regions into darkness for 40 minutes. This fine volcanic material settled over the W side of the mountain and extended to the towns of Basse-Terre and Vieux-Habitants, on the W coast of Guadeloupe 8 km away. The thickness of this grey tephra was very irregular because of the influence of winds: about 8 cm near the summit to 1 or 2 cm near Basse-Terre. This eruption was followed by steam and gases rising from a new fracture 400 m long on the SE flank of the cone. A little avalanche (800 m long) of mud and rocks from this fracture accompanied the eruption.

Since 8 July the pressure of the gases has decreased and the temperature has remained around 96°C, but the volcanic seismicity remains important (300 earthquakes registered 9-20 July). A group of scientists from IPG, Commissariat à l'Energie Atomique, and the Université de Paris Sud, is investigating this eruption. They concluded that the eruption is phreatic (like the eruptions in 1956, [1837-38], and 1797). The chemical composition of the volcanic sand is the same as that of 1956 and corresponds to the composition of the old material of the cone (SiO2 = 57.8%). No new magma was emitted during this eruption.

Addendum: Summary of eruptive and seismic activity 25 July-1 September. Earthquake hypocenters are given in kilometers below sea level unless otherwise noted. [Corrections and additions to this addendum supplied by J. Gautheyrou and LANL, originally printed in 1:11, have been incorporated here.]

25 July: Significant ash eruption.

09 August: Ash eruption, causing a small river to stop flowing for 24 hours. When flow resumed, the water was very muddy.

12 August: Powerful new ash eruption containing juvenile material [but see 1:12]. Evacuation of 72,000 persons began (figure 3); evacuation was completed 15 August.

Figure 3. Geologic map of Soufrière Guadeloupe volcano, after Catalog of Active Volcanoes of the World. Heights are in meters. The area below the dashed line is the section of Basse-Terre that was evacuated due to the possibility of a major eruption. The crosses indicate the locations of the USGS dry-tilt stations at Savane à Mulets (closest to the summit), Parnasse, and Bonne Terre (farthest from the summit).

16 August: Very fine ash erupted from the fissure that opened 8 July. At 1730 a magnitude 4.6 earthquake with a hypocenter at about 2.5 km occurred, followed by 20 minutes of very frequent tremors that saturated a detector 8 km from the volcano for about 10 minutes.

17 August: Approximately 900 earthquakes were recorded in the 24 hours after the beginning of the 16 August seismic crisis. Depths of focus ranged from 1 to 3 km. An earthquakes registering about 4.0 occurred at 2315. An expedition to the volcano noted weaker gas pressure and a new 5-cm ashfall at the foot of the dome. Mudflows were forming from the new ash because of heavy rainfall. At 1700 the principal vent was puffing and a plume of fine particles was being emitted from the N fracture. The 1,500 residents of Vieux-Fort were evacuated. Microprobe analysis of earlier 1976 ejecta indicated andesitic magma at ~900°C.

18 August: The volcano was quiet enough to allow the temporary return of farmers. Earthquake foci were about 2.5 km deep.

19 August: About 1 mm of fine dust was found on the dome. 95% of the erupted material was <0.2 mm in diameter; the coarsest was 2 mm mushroom-colored glass. Dust made breathing difficult in a sector from Basse Terre to Bouillante. Earthquake hypocenters were at about 2.5 km depth.

20 August: There was a steady, non-explosive emission of steam rising to <300 m.

21 August: A major increase in the SO2 content of gases sampled was followed in about 8 hours by 11 minutes of harmonic tremor, beginning at 2326. All instruments were saturated for the first 3 minutes. An ash eruption, probably coinciding with the harmonic tremor, left a few centimeters of ash at the base of the dome, 3 mm 1/3 of the way up the mountain, and ~1 mm on the S coast. An expedition the following day discovered that the SE fracture had been widened and that blocks up to 1 m across had been blown 400 m to the old rim (L'Echelle). Hypocenters of recorded earthquakes were at or above sea level.

22 August: More than 100 of the 156 recorded earthquakes occurred by 0800. Activity then declined. Emission of steam and other gases occurred from vents south of the summit dome (Gouffre Tarissan, Pont Chinois and Gouffre Dupuy). Rain caused a mudflow in the Galion River.

23 August: An increase in radon emission during the afternoon predicted an increase in activity; minor dust emissions were reported.

24 August: A period of major seismic activity began at 0256 with a M 4.1 event centered 2 km under the W side of Soufrière. More than 1,000 earthquakes were recorded by 1530 (figure 4), two of which were felt in Pointe-a-Pitre, 20 km away. Intervals between events and earthquake amplitudes were both decreasing by afternoon. Radon percentage in the gas increased with increased seismicity. SO2 had returned to normal. Minor dust emission continued. 50 cm of dust, largely composed of fresh glass, was present at the S side of the summit dome (Gouffre Tarissan).

Figure 4. Number of recorded seismic events per day at Soufrière Guadeloupe, 21 July-7 November 1976.

25 August: The volume of ash erupted increased significantly and the eruption clouds were much darker after 1530. Ash emission was from the S and E vents (Gouffre Tarissan and Dent de l'Est). Study of the tephra erupted since the 24 August seismic crisis indicates both an increase in the percentage of fresh glass and an increase (to 2 mm) in the size of the glass shards. The percentage of chemical weathering products in the ejecta also increased. Between 2000 on 25 August and 0600 on 26 August, 120 earthquakes were recorded, some having hypocenters as shallow as 300 m above sea level. Gas analyses showed lower percentages of SO2, SO3, and H2S than for previous days. Radon again increased during seismic crises.

26 August: A 100-200 m column of ash was erupted continuously from Gouffre Tarissan (the main vent at the top of the dome) and from the upper end of the SE fracture. The remainder of the SE fracture emitted steam that was almost entirely of meteoric origin. The 26 August ash was dry, and therefore paler than the wet ash of 25 August. The ash was blown W; 2 cm were deposited on the W slopes of the dome and 1-2 mm on the W coast towns. Approximately 50% of the ash was juvenile glass [but see 1:12]. Ash emission ended in the morning. The magmatic component of the emitted gases was low.

27 August: Considerable steam was emitted, along with some dust. Fresh glass was erupted from Pont Chinois and the N fracture. SO2 and H2S were present in small amounts in the volcanic gases.

28 August: An expedition to the dome found 1 m of very fine dust around Gouffre Tarissan and a few centimeters of dust along the flanks of the dome. One block a few centimeters across was found near the top of the dome.

29 August: A 10 µrad inflation of the volcano had occurred since 28 August. Eruptive activity was limited to minor ash emission. Earthquake hypocenters 27-29 August were all shallower than 3 km; all but four were shallower than 2 km, and one was above sea level. No ash emission occurred 28-29 August. The gases analyzed were almost entirely of meteoric origin.

30 August: A small eruption occurred at 1015 from the main vent, accompanied by 22 minutes of harmonic tremor, the first 13 minutes of which saturated the instruments. A party of seven volcanologists was showered by blocks up to 1 m across; four were injured but none seriously. 209 earthquakes were recorded. The ash, analyzed by the LANL, is 95% alteration products (fine-grained clayey material and pyrite) and 5% rock and crystal fragments (andesite, plagioclase, and pyroxene). Volatile content was high, and there was no fresh glass.

31 August: Large volumes of steam with some admixed ash erupted from all of the previously active vents. The steam cloud from the main vent reached 2,000 m altitude in the evening due to light winds. 6-8 cm of juvenile ash (80% glass), which flocculated into 5 mm flakes as it fell, was deposited near the main vent, as were blocks up to 20 cm across that were torn from the vent and blown up to 400 m away. A new earthquake swarm began at 1035 and lasted for 6-8 hours, accounting for most of the 249 seismic events recorded 31 August. A total of 5989 earthquakes were recorded in August, 43 of which were felt.

1 September: Strong steam emission continued, producing cauliflower clouds that reached a height of 300 m before being blown W. A grayish-brown haze of very fine ash was falling on the top quarter of the volcano.

Information Contacts: J. Dorel, IPG, Paris; J. Gautheyrou, ORSTOM; J. Tomblin, UWI; M. Feuillard, Lab. de Physique du Globe; LANL.
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08/1976 (NSEB 01:11) Summary of activity during 2-15 September 1976

2 September: Heavy steam emission from all vents continued after the 30 August eruption. Ash emission was slight. Several loud, booming reports were heard in rapid succession at 1600.

3-7 September: Surface activity diminished. No significant ash eruption occurred. Tilt measurements showed a very slight movement downwards to the NW through 5 September; a 2-3 µrad deflation was noted between 6 and 7 September. Mean earthquake focal depth increased to ~3 km.

7-9 September: Eruptive activity was limited to mild steaming. Gas analysis yielded low values for acid gases (SO2, F2, and fluorides). The magnetic anomaly increased slightly. Mean focal depths were 2.5 km (based on 4 events) on 8 September, increasing to 3.4 km (based on three events) on 9 September.

10-13 September: Mild steaming continued; only small amounts of gases other than H2O were present. At 0418 on 13 September a M 3 earthquake occurred, centered under St. Claude (SW of the summit).

14 September: A summit eruption, lasting between 5 and 9 minutes, began at 1922, 15.4 days after the last significant eruption. Juergen Kienle (University of Alaska) had predicted an eruption between 14 and 18 September, a period centered around the lunar last quarter on 16 September. Immediately prior to the eruption, tilt at the summit went off scale. Loud noise was heard, but cloud cover at the summit prevented visual observation. Harmonic tremor accompanied the eruption, saturating seismographs for the first 4 minutes. Inspection of the summit area revealed airfall ash as far away as St. Claude (4.5 km SW of the summit) and Vieux Habitants (11 km W of the summit). Tom McGetchin reported that a small directed blast, originating from a fissure just S of the main vent, defoliated vegetation up to 500 m away.

15 September: Eruptive activity was confined to steaming and minor ash emission.

Local seismic energy release from mid-July to mid-September was calculated at the University of the West Indies (table 1).

Table 1. Total local earthquake energy for each of six 10-day periods and one 8-day period, 8 July-13 September 1976. Calculated using the formula log E = 9.4 + 2.14 M + 0.054 m2 by the Seismic Research Unit, University of the West Indies.

         1976      Total Local Earthquake Energy (Ergs)

    08 Jul-17 Jul  3.0  x 10^17 (Initial steam explosion 8 July)
    18 Jul-27 Jul  6.3  x 10^17
    28 Jul-06 Aug  1.6  x 10^18
    07 Aug-16 Aug  2.27 x 10^19 (Evacuation began 12 August)
    27 Aug-05 Sep  1.72 x 10^19
    06 Sep-13 Sep  4.63 x 10^16 (8-day period)

Dry tilt stations were installed 28 August by the USGS and are being relevelled daily by George Jezouin, government engineer (table 2).

Table 2. Data from three USGS dry tilt stations on the SW flank of Soufrière, August-September 1976. All values are expressed in µrad vectored towards or away from the summit. Positive values represent inflation.

                       Bonne Terre   Parnasse   Savane à Mulets

    Azimuth to Summit:    N47°E        N66°E         N10°E
    Distance to Summit:   5 km         3 km          1 km

    DATE
    29 Aug               10 µrad inflation; no station data
    31 Aug                -4.1         -7.0         +32.0
    02 Sep                 0.0         +5.0          -9.0
    03 Sep                +3.0         -4.0          -6.0
    04 Sep                -3.0         -6.0          -4.5
    06 Sep                +5.0         -4.0          +2.5
    07 Sep                 0.0         -7.0           --
    08 Sep                -3.5         -5.0           0.0
    09 Sep                +2.3         +3.8           --
    10 Sep                     Deflation; no figures
    12 Sep                     Inflation; no figures
    13 Sep                     Inflation; no figures
    14 Sep                +5.0          0.0           0.0

Raw data from the LANL borehole tiltmeter array appear to be generally compatible with the dry tilt figures. 5-10 µrad tilt events occurring over about 10-minute time spans have been recorded simultaneously at more than one tilt station.

Seismic velocity profiles (18 shot points on land, 2-3 in the ocean) were being run 16 and 17 September by a French team. Velocities previously used to calculate focal depths were estimates which may have been too high. The French scientific team is responsible for gas sampling, magnetic readings and seismic recording as well as overseeing all scientific work on the volcano. The LANL is operating a camera station at Fort St. Charles and plans to establish another at Pointe-a-Pitre. Juergen Kienle is running a daily gravity survey. Michael Sheridan (Arizona State Univ.) is studying pyroclastic flow deposits from past eruptions.

Information Contacts: J. Tomblin and W. Aspinall, UWI; T. McGetchin, LANL.
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09/1976 (NSEB 01:12) Variable activity continues; ash eruption on 22 September

16 September: Heavy steaming occurred from the S and SE sides of the summit dome. Differential magnetometer readings increased at the summit and decreased at Matouba with respect to a base station at Basse Terre.

17-19 September: Large inflation was shown by LANL tilt stations to continue through the 18th. Deflation was observed by the same stations on the 19th. Sulfur was noted in the gases on the 18th. Eruptive activity was minor.

20 September: A seismic event occurred at 0100. LANL reports that the tilt, gravity, differential magnetometry, and seismicity each showed distinctive patterns prior to this event, similar to the patterns noted before the 14 September activity. These data have yet to be interpreted in terms of a magma chamber model. LANL noted approximately 10 µrad inflation at the summit, and ~5 µrad deflation at lower tilt stations during the the 24 hours after the event.

21 September: Eruptive activity was minor.

22 September: An ash eruption, producing a 3,500-m cloud, occurred at 0645, accompanied by 18 minutes of harmonic tremor, 6 minutes of which saturated seismographs. About 1 cm of ash fell downwind at Baillif-Vieux-Habitants. Ash was sampled from a 1-mm deposit near the S edge of the ashfall area.

23 September: Strong steaming, possibly with some ash emission, was occasionally visible through heavy clouds.

24-27 September: The activity stabilized to moderate steaming and minor ash emission. LANL recorded a large tilt episode, beginning at 2300 on the 27th and lasting several hours.

28 September: A 300-m plume was visible for much of the day. At 1010 an earthquake occurred that was felt in Pointe-a-Pitre. Seventy minutes later, LANL recorded the beginning of deflation. The tilt and seismic data are thought by LANL to indicate cavity collapse.

29 September: LANLLASL reported the beginning of inflation at 1445, then deflation at 1745.

30 September: A 20-minute period of tremors began at 0002. Two large and four small events were recorded. Cavity collapse was again suggested by LANL as an explanation for the seismic episode.

In other tilt experiments, R.S. Fiske and W.T. Kinoshita, supported by the USGS, SI, and OFDA, established four dry-tilt arrays on the SW flank of Soufrière in late August. These four arrays are at about 1, 3, 4, and 5 km from the summit. More than 25 reoccupations of these arrays (29 August-30 September) by French technicians have indicated daily station "noise" sometimes exceeding 5 µrad, but the suggestion of true volcano inflation has been recorded only at the station 5 km from the summit. The bulk of the dry-tilt data gathered to date therefore do not indicate that the volcano is being deformed as a result of the inflation of a magma reservoir. This tentative conclusion is supported by measurements of P.A. Blum, who installed two pendulum-type tiltmeters at the now abandoned volcano observatory about 3 km from the summit. These tiltmeters, capable of detecting changes in ground tilt of a few parts in 108, have indicated tilt changes of only fractions of a µrad from 25 September, when measurements were begun, to 29 September. Neither of these observations, however, has been made over times that would record the short periods of tilt reported by LANL during the hour preceding small eruptions.

[Magnetic variations measured on the volcano in September were positive at all but one station, and intense, reaching 6nT at the end of the month (Zlotnicki, 1986).]

Earlier reports of fresh volcanic glass in the ejected ash from La Soufrière are now regarded to have been in error. There is no confirmed evidence that juvenile magma has reached the surface.

Information Contacts: W. Aspinall and J. Tomblin, UWI; LANL; J. Gautheyrou, ORSTOM; R. Fiske, SI.
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10/1976 (NSEB 01:13) Eruption on 2 October deposits ash 7 km away; continued steam emission

2 October: At about 1630, a steam and ash eruption began, producing a cloud that reached a maximum of 1000-1500 m height. The cloud deposited a fine veneer of ash on vegetation as far as 7 km downwind. Maximum ejecta diameter on the summit dome was 1-2 cm. Mudflows accompanied the eruption. Harmonic tremor events of 10 and 13 minutes respectively saturated seismographs at 1615 and 1654.

3 October: Normal activity resumed (200-300-m sulfurous steam plumes).

4 October: Steam clouds, fluctuating in volume and ash content, were emitted from the dome fracture system. Activity was greatest near the S flank. Ash slurries, 4-5 m wide, flowed downslope from the dome fractures. Two ash samples and one mudflow sample were taken by LANL the next day.

5 October: Summit fumarolic activity was visible in the early morning and late afternoon. Little or no ash was present in the steam plumes.

6-7 October: Clouds and heavy rain precluded observations of the summit area.

8 October: Moderate steam plumes, sometimes containing small amounts of ash, were emitted during the morning. A significant increase in activity began at 1237, about 2.5 hours after unusual heavy rains on the summit area. The steam plumes reached 50 m height.

9 October: Continued moderate steam emission, with varying but minor amounts of ash in the plumes.

10 October: At 1111, a 13-minute period of harmonic tremor began, coincident with a pronounced increase in ash emission from the summit, which lasted for 20-30 minutes. Four mm of ash were deposited at the summit parking lot and at Marigot (5.5 km W of the summit), considerably more than was deposited from the larger ash clouds of 2 and 4 October.

11 October: A pronounced increase in seismic activity began at about 0500 and continued through about 1100. No simultaneous increase in eruptive activity was noted.

12 October: Eruptive activity was limited to weak steaming. Plumes rose only 10-12 m above the summit.

13-14 October: Steam emission returned to the "moderate" level of 8-9 October.

15 October: LANL scientists returned to Los Alamos leaving borehole tiltmeters in concrete building foundations for continued use by the French team.

21 October: 65 earthquakes were recorded.

22 October: Earthquake activity increased sharply. Between 1330 and 1610, 182 earthquakes larger than M 2.2 were recorded. Eruptive activity increased during the afternoon and evening.

23 October: A harmonic tremor event occurred at about 0530, saturating instruments for 1 minute. Steam and "smoke" emission had declined since the previous evening.

Continuing dry tilt measurements by French technicians have indicated no coherent pattern of deformation 1-16 October. It is probable that the small tilts observed can be attributed to the near-surface effects of variation in rainfall, sunlight, and evaporation at each of the 4 stations.

Analysis of unsieved material by LANL from the 30 September and 15 October eruptions detected mainly hydrothermally altered lithic and mineral fragments. No fresh glass was found (table 3).

Table 3. Modal analyses by LANL of unsieved 30 September and 15 October 1976 ejecta from Soufrière.

    Components (%)            30 Sep 1976   15 Oct 1976

    Altered and unaltered
      plagioclase, ortho-          18            16
      and clinopyroxe
    Altered and unaltered
      lithic fragments             18            20
      (mostly porphyritic,
      glassy dacite)
    Altered colorless glass         4             1
    Matrix; <2 µm altered
      glass and mineral            55            60
      phases, clay, and
      celadonite (?)

Sulfur contents of tephra samples increased over the period mid-August to early September, according to LANL analyses (table 4).

Table 4. Sulfur content of several ash samples from August 1976 eruptions of Soufrière. Analyzed by D. Curtis, LANL, using the thermal neutron-prompt gamma activation method.

    1976     Wt.% sulfur of tephra samples

    12 Aug   1.7
    22 Aug   2.3 (1.1, 3.4; two locations)
    26 Aug   2.7
    27 Aug   3.6 (3.0, 4.1; two locations)
    30 Aug   4.3

Information Contacts: LANL; J. Gautheyrou, ORSTOM; AFP.
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11/1976 (NSEB 01:14) Phreatic explosions and mild steaming; evacuation ends 1 December

30 October: A 9-minute phreatic explosion occurred at about 1000. At 2238 a period of volcanic tremor began.

1 November: Phreatic explosion at about 1100.

6 November: Phreatic explosion at about 2200. The periods between phreatic explosions were characterized by mild steaming from fissures on the summit dome.

On 15-18 November, CNRS convened a committee of scientists in Paris to review the Soufrière situation and to assess the hazard posed by the volcano. This committee was chaired by Frank Press of the U.S., and included the following members: Shigeo Aramaki, Japan; Franco Barberi, Italy; Jean Coulomb, France; Richard S. Fiske, U.S.; Paolo Gasparini, Italy; Claude Guillemin, France; and Gudmundur Sigvaldason, Iceland.

The committee concluded that as of mid-November there was low probability of a dangerous eruption at La Soufrière, but that the situation could change. In order to detect these changes, the committee recommended an augmented program of study that included increased geological and petrological observation of the volcano and its ejecta, expansion of the deformation studies (precise levelling and tiltmetry), monitoring of volcanic gases, and expansion and improvement of seismic monitoring procedures. The committee report also outlined a possible model explaining the volcano's behavior. The model calls for the tectonic fracturing of hot rock or partly solidified magma beneath the volcano. This fracturing permitted the rapid influx of groundwater, of both meteoric and marine origin, which was then heated and driven off in copious outpourings of steam from the summit of the volcano. At times, steam was expelled with such violence that particles of pre-existing, altered rock were torn from the interior of the volcano and ejected to form airborne clouds of ash.

Several hours after the release of the committee report on 18 November, the French Government announced that the evacuation on Guadeloupe would end, and that the last of the 72,000 evacuees could return to their homes on 1 December.

Information Contacts: M. Feuillard, Lab. de Physique du Globe; J. Dorel, IPG, Paris; R. Fiske, SI.
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12/1976 (NSEB 01:15) Mild steaming with an occasional weak phreatic explosion

Activity has declined to mild steaming with an occasional weak phreatic explosion.

Information Contacts: J. Gautheyrou, ORSTOM.
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01/1977 (NSEB 02:01) Summary of steam-and-ash explosions during October 1976-January 1977

Significant steam and ash explosions after 11 October occurred 30 October, 1, 6, and 7 November, and 5, 13, 14, 15, 17, 19, and 30 January [but see 2:2]. Two harmonic tremor events were recorded on 1 November and one on 6 November. No information on harmonic tremor is available after 7 November. [Both the number of earthquakes and seismic energy release declined after mid-November (table 5).]

Table 5. Number of earthquakes and total seismic energy release at Soufrière Guadeloupe, October 1976-May 1977. Courtesy of M. Feuillard.

                 Number of    Total Seismic Energy
       1976     Earthquakes      (x 10E13 ergs)

    01-10 Oct       412              446
    11-20 Oct       895              532
    21-31 Oct      1008              929
    01-10 Nov       489              523
    11-20 Nov       235              402
    21-30 Nov       316              168
    01-10 Dec       204              225
    11-20 Dec       102              165
    21-31 Dec        93               41
    01-10 Jan        69               76
    11-20 Jan       126               71
    21-31 Jan       116              154
    01-10 Feb        76              152
    11-20 Feb        86               38
    21-28 Feb        17               32
    01-10 Mar        23                4
    11-20 Mar        65               54
    21-31 Mar        66               52
    01-10 Apr        12                2
    11-20 Apr        28                6.9
    21-30 Apr         6                1.1
    01-10 May         5                0.9
    11-20 May         9                1.7

Information Contacts: M. Feuillard, Lab. de Physique du Globe.
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02/1977 (NSEB 02:02) Phreatic activity continues; large explosion on 29 January

"Phreatic activity has continued at La Soufrière through 23 February. The largest explosion of the 1976-77 activity occurred at 1911 on 29 January 1977 and was heard by people living as far as 10 km from the summit. Lithic blocks as large as 0.5 m in diameter were thrown 1 km from the summit fissures. Five centimeters of ash was deposited at Savane à Mulets and 5 mm of ash fell on Matouba, 3 km W of the summit. Smaller phreatic explosions occurred on 13 and 15 February, and measurable amounts of ash were erupted on 5, 7, and 10-15 February. On 23 February only minor amounts of steam were being emitted from the volcano.

"In contrast to the eventful phreatic activity of recent weeks, the local seismicity has continued to decline. Only 6-10 earthquakes/day were detected 1-23 February and a felt event occurs only once in every 10 days.

"Petrographic study continues to confirm that ejecta from Soufrière consist only of older, altered material. No fresh glass has been observed. As before, ground deformation measurements with various types of tiltmeters (pendulum, borehole, dry tilt) have indicated no significant changes in the overall shape of the volcano."

Information Contacts: R. Fiske, SI.
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03/1977 (NSEB 02:03) Earthquake rate decreases to 1 per day

"Daily recorded earthquakes at Soufrière had decreased from a maximum of 1257 on 24 August 1976 to one per day by the first week in March 1977 (figure 5). Figure 6 shows the seismic energy released during 10-day periods. Total energy release from 1 November 1975 through February 1977 was ~1.9 x 1018 ergs. Figure 7 shows the number of earthquakes in various magnitude ranges. The largest magnitude was 4.2 (4.9 by NEIS determination) on 16 August 1976.

Figure 5. Daily recorded earthquakes at Soufrière Guadeloupe, October 1975-March 1977. Courtesy of J. Dorel.
Figure 6. Seismic energy release in ergs for 10-day periods at Soufrière Guadeloupe, July 1975-February 1977. Courtesy of J. Dorel.
Figure 7. Number of recorded earthquakes at Soufrière Guadeloupe in magnitude increments of 0.5, late 1975-February 1977. Courtesy of J. Dorel.

"Hypocenter determination has been made for about 350 events. Figure 8 shows NW-SE and NE-SW vertical sections (under the volcano) onto which the foci are projected. Different symbols are used for different time series, but the variation with time of the depths of quakes during the crisis is not meaningful. Mean depth is about 2.5 km.

Figure 8. Cross-sections at Soufrière Guadeloupe running NW-SE (top) and NE-SW (bottom) showing earthquake hypocenters. Courtesy of J. Dorel.

"Volcanic tremor, the duration of which varied from a few minutes to a few tens of minutes, has been recorded by the seismographs. The tremor events correspond to such important surface manifestations as steam, solid ejecta, and fracture opening. With its 16,000 earthquakes and a total energy release greater than 1018 ergs, the La Soufrière crisis is the most important in the Carribean region in the past 40 years."

Information Contacts: J. Dorel, Univ. Pierre et Marie Curie, Paris.
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04/1977 (NSEB 02:04) Decreased seismic and surface activity

Surface and seismic activity have declined considerably at Soufrière since the peak of the volcano-seismic crisis in August 1976 (table 5). The most recent phreatic explosion occurred on 1 March, after which solfataric activity continued into April from the uppermost craters but diminished on the flank and in the Col de l'Echelle, just SE of the summit dome. Ash was emitted for portions of 20 days 1 January-15 April.

Information Contacts: M. Feuillard, Lab. de Physique du Globe.
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05/1977 (NSEB 02:05) Fumarolic activity

Surface activity at La Soufrière remained entirely fumarolic, and was strongest from the fissures toward the top of the summit dome. [Seismicity continued an irregular decline (table 5).]

Information Contacts: M. Feuillard, Lab. de Physique du Globe.
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06/1977 (NSEB 02:06) Summary of seismicity since mid-1975

Table 6 summarizes seismicity at Soufrière from mid-1975 through May 1976.

Table 6. Total seismic energy release (x 1013 ergs) per 1/3-month period, July 1975-May 1977. Courtesy of M. Feuillard.

    Days of Month   01-10   11-20   21-end of month

    Jul 1975           0        0            23
    Aug                0        0             0
    Sep                0        0             0
    Oct                0        0             1
    Nov                0        1            91
    Dec                0        0            14
    Jan 1976           0        0             1
    Feb                1        7             5
    Mar                1      100         18000
    Apr              175       26           125
    May               35      150          4600
    Jun              380       88            64
    Jul               80      510           768
    Aug             1544    33831         20010
    Sep             1027      469           949
    Oct              446      532           930
    Nov              523      402           168
    Dec              225      165            41
    Jan 1977          76       71           154
    Feb              152       38            33
    Mar                4       54            52
    Apr                2        7             1
    May                1        2             6

Further References. Feuillard, M., Allegre, C.J., Brandeis, G., Gaulon, R., and others, 1983, The 1975-1977 crisis of La Soufrière de Guadeloupe (F.W.I.): A still-born magmatic eruption: JVGR, v. 16, p. 317-334.

Information Contacts: M. Feuillard, Lab. de Physique du Globe.
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10/1981 (SEAN 06:10) Temperature, magnetic field stable

IPG geophysicists have installed three telemetering magnetometers and established a network of 20 additional non-telemetering magnetometer stations on the flanks of Soufrière. Although significant changes in the magnetic field were recorded over periods of a few [months] during the phreatic and seismic activity of 1976-77, no variations of more than 1.5 nT were detected between August 1980 and March 1981.

IPG geophysicists also drilled two boreholes, to 77 m depth in the summit dome, and to 97 m depth immediately beside the dome. The temperature measurement at the bottom of dome borehole decreased steadily, from 97.5°C in April 1978 to 87°C in December 1980. . . . No significant temperature variation was recorded in the borehole near the dome, which remained at about 19°C through 1980. The temperature of a fumarole (Lacroix) about 80 m below the summit dropped from about 160°C in July 1978 to just over 100° by January 1979 and has remained between 96° and 98°C in 1981.

Further Reference. Zlotnicki, J., 1986, Magnetic measurements on La Soufrière volcano, Guadeloupe (Lesser Antilles), 1976-1984: A re-examination of the volcanomagnetic effects observed during the volcanic crisis of 1976-1977: JVGR, v. 30, p. 83-116.

Information Contacts: J. Pozzi, J. Zlotnicki, G. Simon, J. Le Mouel and J. Cheminée, IPG, Paris.
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01/1982 (SEAN 07:01) Temperatures and chemistry of thermal springs

Since January 1979, samples have been collected 2-3 times per month from six springs with water temperatures of 25-69°C, 0.5-3.5 km from the summit dome. Water temperatures and chemistry remained nearly constant at five of the six springs, as shown by the following maximum variations recorded at any one spring in the nearly 3 years of sampling: temperature (°C) 4%, pH 5%, Cl 20%, HCO3 25%, F 25%. These variations were independent of rainfall and apparently random.

However, Carbet l'Echelle spring, the hottest and nearest to the summit (0.5 km) showed appreciable changes during the survey period. Its water temperature dropped from 69°C in January 1979 to 57° in November 1981, while the concentration of HCO3 ions approximately doubled and large variations in Cl concentrations occurred (figure 9).

Figure 9. Changes in temperature (°C, dashed line), Cl concentrations (10-3 moles/liter, solid line), and HCO3 concentration (10-3 moles/liter, dotted line) for Carbet l'Echelle spring, 500 m from the summit of Soufrière Guadeloupe, January 1979-October 1981.

Information Contacts: S. Bigot, Lab. de Géochemie, Paris; G. Hammouya, Lab. de Physique du Globe; J. Le Mouel and J. Cheminée, IPG, Paris.
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03/1983 (SEAN 08:03) Water temperatures and chemistry

A study of the geochemical evolution of Carbet l'Echelle spring, continued during 1981 and 1982 (figure 10). The water temperature decreased from 62.5°C in January 1981 to 50° in September 1982, while the concentration of HCO3 ions continued to increase (+ 30%). Moreover, although large variations in Cl concentration have been observed since 1979, the background level of Cl began to fall in September 1981 and was reduced by half in one year. Likewise, the concentration of F ions, which has oscillated around a constant value since the beginning of the survey, decreased slightly in late 1982. Water temperatures and chemistry remained nearly constant at the other springs monitored by this study.

Figure 10. Changes in temperature (°C), HCO3 and Cl concentration (103 moles/liter), and F concentration (105 moles/liter) for Carbet l'Echelle spring, 500 m from the summit of Soufrière Guadeloupe, January 1981-September 1982.

Further References: Bigot, S., and Hammouya, G., 1987, Surveillance hydrogéochimique de la Soufrière de Guadeloupe, 1979-1985: Diminuition d'activité ou confinement?: C.R. Acad. Sci. Paris, t. 304, Série II, no. 13, p. 757-760.

Observations volcanologiques: Rapport d'Activite des Observatoires Volcanologiques des Antilles (Guadeloupe-Martinique) - November 1976-April 1977, April 1977-December 1978, 1979, 1980, 1981, 1982, and 1983-1984: Institut de Physique du Globe, Paris.

Information Contacts: S. Bigot, Lab. de Géochemie, Paris; G. Hammouya, Lab. de Physique du Globe; J. Le Mouel, J. Cheminée, IPG, Paris.
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La Soufrière de la Guadeloupe volcano occupies the southern end of Basse-Terre, the western half of the butterfly-shaped island of Guadeloupe. Construction of the Grand Découverte volcano about 0.2 million years ago (Ma) was followed by caldera formation after a plinian eruption about 0.1 Ma, and then by construction of the Carmichaël volcano within the caldera. Two episodes of edifice collapse and associated large debris avalanches formed the Carmichaël and Amic craters about 11,500 and 3100 years ago, respectively. The presently active La Soufrière volcano subsequently grew within the Amic crater. The summit consists of a flat-topped lava dome, and several other domes occur on the southern flanks. Most historical eruptions have originated from NW-SE-trending fissure systems that cut across the summit and upper flanks. A relatively minor phreatic eruption in 1976-77 caused severe economic disruption when Basse-Terre, the island's capital city, which lies immediately below the volcano, was evacuated.

Summary of Holocene eruption dates and Volcanic Explosivity Indices (VEI).

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
1976 Jul 8 1977 Mar 1 Confirmed 2 Historical Observations SE side of summit (Gouffre Tarissan)
1956 Oct 19 1956 Oct 27 Confirmed 1 Historical Observations ESE side, Napoléon Crater
[ 1903 ] [ Unknown ] Uncertain 2   SE side summit dome
1836 Dec 3 1837 Feb 12 Confirmed 2 Historical Observations SE to NW sides of summit dome
1812 Apr 1812 May 10 Confirmed 1 Historical Observations E-W fissure on summit dome
1797 Sep 29 1798 Apr 26 (?) Confirmed 2 Historical Observations NNW side of summit dome
1696 Apr Unknown Confirmed 1 Historical Observations North side of summit dome
1690 Apr 5 (in or after) Unknown Confirmed 1 Historical Observations Gouffre Dupuy, Gouffre Tarissan
1600 ± 50 years Unknown Confirmed   Radiocarbon (corrected)
1440 ± 100 years Unknown Confirmed 4 Radiocarbon (corrected) La Soufrière
1370 ± 150 years Unknown Confirmed 4 Radiocarbon (corrected)
1340 ± 50 years Unknown Confirmed 3 Radiocarbon (corrected)
0370 ± 75 years Unknown Confirmed   Radiocarbon (corrected) La Citerne and L'Eschelle cones
0580 BCE (after) Unknown Confirmed 2 Radiocarbon (uncorrected) South flank (Morne Lenglet)
0820 BCE ± 100 years Unknown Confirmed 3 Radiocarbon (corrected) Morne Amic ?
0980 BCE ± 200 years Unknown Confirmed   Radiocarbon (corrected)
1310 BCE ± 150 years Unknown Confirmed 3 Radiocarbon (corrected) Morne Amic
1810 BCE ± 150 years Unknown Confirmed   Radiocarbon (corrected)
[ 2050 BCE (?) ] [ Unknown ] Uncertain    
3310 BCE ± 150 years Unknown Confirmed   Radiocarbon (corrected) South flank (Gros Fougas)
6450 BCE ± 150 years Unknown Confirmed   Radiocarbon (corrected)
7490 BCE ± 150 years Unknown Confirmed   Radiocarbon (corrected)

This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.


Cones

Feature Name Feature Type Elevation Latitude Longitude
Carmichaël Stratovolcano 1414 m 16° 3' 0" N 61° 40' 0" W
Citerne, La Pyroclastic cone 1115 m 16° 2' 0" N 61° 39' 0" W
Eschelle Pyroclastic cone 1397 m 16° 3' 0" N 61° 39' 0" W
Grande Découverte, La Stratovolcano 1263 m 16° 4' 0" N 61° 40' 0" W
Gros Fougas Pyroclastic cone 801 m 16° 1' 0" N 61° 39' 0" W
Lenglet, Morne Pyroclastic cone 722 m 16° 1' 0" N 61° 40' 0" W
Trois Rivières-Madeleine Volcanic field 801 m 16° 1' 0" N 61° 39' 0" W

Craters

Feature Name Feature Type Elevation Latitude Longitude
Amic Crater 1343 m 16° 3' 0" N 61° 40' 0" W
Gouffre Dupuis Crater 1450 m 16° 3' 0" N 61° 40' 0" W
Gouffre Tarissan Crater 1450 m 16° 3' 0" N 61° 40' 0" W
Napoleon, Cratere Crater 1400 m 16° 3' 0" N 61° 40' 0" W

Domes

Feature Name Feature Type Elevation Latitude Longitude
Amic, Morne Dome 1343 m 16° 3' 0" N 61° 40' 0" W
Dongo, Morne Dome 486 m 16° 2' 0" N 61° 37' 0" W
Madeleine Dome 972 m 16° 1' 0" N 61° 38' 0" W
Soufrière, La Dome 1467 m 16° 3' 0" N 61° 40' 0" W

Thermal

Feature Name Feature Type Elevation Latitude Longitude
Carbet, Fumerolles du Fumarole 1300 m 16° 3' 0" N 61° 39' 0" W
Chaudieres, Les Thermal 1264 m 16° 3' 0" N 61° 39' 0" W
Colardeau, Fumerolles Fumarole 1318 m 16° 3' 0" N 61° 40' 0" W
Fente du Nord, Fumerolle de la Fumarole 1350 m 16° 3' 0" N 61° 40' 0" W
Lacroix, Fumerolle Fumarole 1350 m 16° 3' 0" N 61° 40' 0" W
Mitan, Morne Thermal 1200 m 16° 3' 0" N 61° 39' 0" W
An ash plume rises above the summit of Soufrière volcano on Guadeloupe Island in October 1976 with the deserted streets of Basse-Terre, the island's capital city, in the foreground. The 72,000 inhabitants of Basse-Terre had been evacuated since August because of concern of larger eruptions. In November the evacuation was ended.

Photo by Richard Fiske, 1976 (Smithsonian Institution).
Steam pours from a fissure cutting the summit of La Soufrière in September 1976. Intermittent phreatic eruptions had begun in July and continued until March of the following year. This view from the north shows the Les Santes islands at the right and the tip of Dominica Island in the distance.

Photo by Richard Fiske, 1976 (Smithsonian Institution).
An ash column rises above a fissure on the upper NW flank of La Soufrière de la Guadeloupe volcano in October 1976, with the capital city of Basse-Terre in the background. Intermmitent mild-to-moderate phreatic explosions took place from July 8, 1976, to March 1, 1977. Concern about the possibility of a larger eruption prompted the evacuation of the capital city of Basse-Terre from August to November 1976.

Photo by Richard Fiske, 1976 (Smithsonian Institution).
Vehicles laden with possessions are driven down the streets of Basse-Terre in September 1976, during the evacuation of the island's capital city. About 72,000 persons living on the slopes of the volcano were evacuated until November 1976, producing significant economic disruption.

Photo by Richard Fiske, 1976 (Smithsonian Institution).
A steam-and-ash plume from the summit of La Soufrière volcano rises above the deserted streets of Basse-Terre in October 1976. Intense controversy surrounded the evacuation of 72,000 persons living on the flanks of the volcano. The evacuation, which had resulted in major economic and social disruption, was officially ended in November. This eruption ended without catastrophe, unlike another West Indies eruption two decades later, when the evacuated capital city of Montserrat was devastated by pyroclastic flows.

Photo by Richard Fiske, 1976 (Smithsonian Institution).
La Soufrière volcano, the highest in the West Indies, is a complex stratovolcano that dominates the southern end of Basse-Terre, the western half of the butterfly-shaped island of Guadeloupe. A steam-and-ash column rises above the summit in this October 1976 view from the NE at Pointe-a-Pitre, on the isthmus connecting the island segments. The peak at the left (above the sailboat), l'Echelle, is a young cinder cone; the summit itself is a 500-year-old lava dome, and remnants of older collapsed volcanoes are located to its right.

Photo by Richard Fiske, 1976 (Smithsonian Institution).
Steam rises from a 500-year-old lava dome that forms the summit of La Soufrière volcano on Guadeloupe. It was constructed within the 1-km-wide, horseshoe-shaped Amic Crater, whose northern rim is the flat-topped ridge at the extreme left. Amic Crater was the source of a major explosion and debris avalanche about 3100 years ago during an eruption that resembled the 1980 Mount St. Helens eruption. The peak to its right is l'Echelle, a young cinder cone. This September 1976 view is from the west.

Photo by Richard Fiske, 1976 (Smithsonian Institution).
The summit dome of La Soufrière is seen in the center of this October 1976 aerial view from the SW. The peak at the right is l'Echelle, a scoria cone that is thought to have formed about 1500-2000 years ago. Historical eruptions from the volcano have originated from fissures cutting across the summit dome and its upper flanks.

Photo by Richard Fiske, 1976 (Smithsonian Institution).
Scientists unload equipment in October 1976 to measure deformation of the volcanic edifice at Savane à Mulets, on the south side of the summit lava dome. This was one of several tools used to monitor the volcano during the 1976-77 eruption.

Photo by Richard Fiske, 1976 (Smithsonian Institution).
La Soufrière lava dome, forming the summit of Soufrière Guadeloupe volcano, was emplaced at the end of a major eruption that took place around the mid-15th century. The eruption began with collapse of part of a previous lava dome forming a debris avalanche, followed by a major explosive eruption in which dacitic pumice and andesitic banded scoria were sequentially ejected. The eruption concluded with growth of La Soufrière summit lava dome, which is seen here from the north.

Photo by Paul Kimberly, 2002 (Smithsonian Institution).

The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title.

Besson P, Poirier J-P, 1994. The 3100 BP eruption of the Soufriere of Guadeloupe - A transmission electron microscopy study of the cryptodome andesite. Bull Volc, 56: 184-192.

Boudon G, Semet M P, Vincent P M, 1989. The evolution of la Grande Decouverte (la Soufriere) volcano, Guadalope (FWI). In: Latter J H (ed), {Volcanic Hazards - Assessment and Monitoring}, Berlin: Springer-Verlag, p 86-109.

Komorowski J-C, Boudon G, Semet M, Beauducel F, Antenor-Habazac C, Bazin S, Hammouya G, 2005. Guadeloupe. In: Lindsay J M, Robertson R E A, Shepherd J B, Ali S (eds). {Volcanic Hazard Atlas of the Lesser Antilles}, Trinidad and Tobago, Seismic Res Unit, Univ West Indies, p 67-105.

Robson G R, Tomblin J, 1966. West Indies. Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI, 20: 1-56.

Westercamp D, 1980. Une methode d'evaluation et de zonation des risques volcaniques a la Soufriere de Guadeloupe, Antilles Francaises. Bull Volc, 43: 431-452.

Volcano Types

Stratovolcano
Lava dome(s)

Tectonic Setting

Subduction zone
Oceanic crust (< 15 km)

Rock Types

Major
Andesite / Basaltic Andesite
Dacite
Minor
Basalt / Picro-Basalt
Rhyolite

Population

Within 5 km
Within 10 km
Within 30 km
Within 100 km
8,839
71,345
256,899
482,449

Affiliated Databases

Large Eruptions of Soufriere Guadeloupe Information about large Quaternary eruptions (VEI >= 4) is cataloged in the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
WOVOdat WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. It is sponsored by the World Organization of Volcano Observatories (WOVO) and presently hosted at the Earth Observatory of Singapore.
EarthChem EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility Integrated Earth Data Applications (IEDA). IEDA is a collaborative effort of EarthChem and the Marine Geoscience Data System (MGDS).
Smithsonian Collections Search the Smithsonian's NMNH Department of Mineral Sciences collections database. Go to the "Search Rocks and Ores" tab and use the Volcano Name drop-down to find samples.