u.s. geological survey m7.8 coastal ecuador earthquake of...

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U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ^ _ Manizales Ibague Piura Medellin Cali Quito Guayaquil Colombia Ecuador Peru 75° 75° 85° # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * # * ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # # i i i i i i i i i i i i i ^ _ Caribbean Sea Atlantic Ocean Pacific Ocean 78 mm/yr 74 mm/yr 19 mm/yr 20 mm/yr 20 mm/yr 65 mm/yr 58 mm/yr 71 mm/yr 68 mm/yr 61 mm/yr 65° 65° 75° 75° 85° 85° 95° 95° 15° 15° 15° M7.8 Coastal Ecuador Earthquake of 16 April 2016 0 250 500 125 Kilometers ^ _ 65° 65° 75° 75° 85° 85° 95° 95° 0 500 1,000 1,500 250 Kilometers Prepared in cooperation with the Global Seismographic Network Tectonic Setting Seismic Hazard Epicentral Region TECTONIC SUMMARY The April 16, 2016 M 7.8 earthquake, offshore of the west coast of northern Ecuador, occurred as the result of shallow thrust faulting on or near the plate boundary between the Nazca and Pacific plates. At the location of the earthquake, the Nazca plate subducts eastward beneath the South America plate at a velocity of 61 mm/yr. The location and mechanism of the earthquake are consistent with slip on the primary plate boundary interface, or megathrust, between these two major plates. Subduction along the Ecuador Trench to the west of Ecuador, and the Peru-Chile Trench further south, has led to uplift of the Andes mountain range and has produced some of the largest earthquakes in the world, including the largest earthquake on record, the 1960 M 9.5 earthquake in southern Chile. While commonly plotted as points on maps, earthquakes of this size are more appropriately described as slip over a larger fault area. Events of the size of the April 16, 2016 earthquake are typically about 160x60 km in size (length x width). Ecuador has a history of large subduction zone related earthquakes. Seven magnitude 7 or greater earthquakes have occurred within 250 km of this event since 1900. On May 14th, 1942, a M 7.8 earthquake occurred 43 km south of this April 16th, 2016 event. On January 31st, 1906 a M 8.3 earthquake (reportedly as large as M 8.8 in some sources) nucleated on the subduction zone interface 90 km to the northeast of the April 2016 event, and ruptured over a length of approximately 400-500 km, resulting in a damaging tsunami that caused in the region of 500-1,500 fatalities. The April 2016 earthquake is at the southern end of the approximate rupture area of the 1906 event. A shallow, upper crustal M 7.2 earthquake 240 km east of the April 2016 event on March 6th, 1987 resulted in approximately 1,000 fatalities. EXPLANATION Main Shock ^ _ Aftershocks ! ( Earthquake Magnitude ( 5.5 - 6.5 ( 6.5 - 7.0 ( 7.0 - 7.5 ( 7.5 - 8.0 ( > 8.0 Earthquake Depth (km) ! ( 0 - 69 ! ( 70 - 299 ! ( e 300 Finite Fault Model Slip (mm) Ô < 50 Ô 50 - 150 Ô 150 - 250 Ô 250 - 270 Ô 270 - 340 Ô > 340 Plate Boundaries # Subduction Transform Divergent Others Seismic hazard is expressed as peak ground acceleration (PGA) on firm rock, in meters/sec², expected to be exceeded in a 50-yr period with a probability of 10 percent. EXPLANATION Mag e 7.0 ! ( 0 - 69 km ! ( 70 - 299 ! ( 300 - 600 Plate Boundaries # Subduction Transform Divergent Others 0 500 1,000 1,500 250 Kilometers Peak Ground Acceleration in m/sec**2 .2 .4 .8 1.6 2.4 3.2 4.0 4.8 Epicentral Region ^ _ Epicentral Region DATA SOURCES EARTHQUAKES AND SEISMIC HAZARD USGS, National Earthquake Information Center NOAA, National Geophysical Data Center IASPEI, Centennial Catalog (1900 - 1999) and extensions (Engdahl and Villaseñor, 2002) EHB catalog (Engdahl et al., 1998) HDF (unpublished earthquake catalog, Engdahl, 2003) Global Seismic Hazard Assessment Program Volcanoes of the World (Siebert and Simkin, 2002) PLATE TECTONICS AND FAULT MODEL PB2002 (Bird, 2003) Ji, C., D.J. Wald, and D.V. Helmberger, Source description of the 1999 Hector Mine, California earthquake; Part I: Wavelet domain inversion theory and resolution analysis, Bull. Seism. Soc. Am., Vol 92, No. 4. pp. 1192-1207, 2002. DeMets, C., Gordon, R.G., Argus, D.F., 2010. Geologically current plate motions, Geophys. J. Int. 181, 1-80. BASE MAP NIMA and ESRI, Digital Chart of the World USGS, EROS Data Center NOAA GEBCO and GLOBE Elevation Models REFERENCES Bird, P., 2003, An updated digital model of plate boundaries: Geochem. Geophys. Geosyst., v. 4, no. 3, pp. 1027-80. Engdahl, E.R., and Villasenor, A., 2002, Global Seismicity: 1900-1999, chap. 41 of Lee, W.H.K., and others, eds., International Earthquake and Engineering Seismology, Part A: New York, N.Y., Elsevier Academic Press, 932 p. Engdahl, E.R., Van der Hilst, R.D., and Buland, R.P., 1998, Global teleseismic earthquake relocation with improved travel times and procedures for depth determination;Bull. Seism. Soc. Amer., v. 88, p. 722-743. EARTHQUAKE SUMMARY MAP NAZCA PLATE PAGER Distribution of the amplitude and direction of slip for subfault elements of the fault rupture model are determined from the inversion of teleseismic body waveforms and long period surface waves. Arrows indicate the amplitude and direction of slip (of the hanging wall with respect to the foot wall); the slip is also colored by magnitude. The view of the rupture plane is from above. The strike of the fault rupture plane is 29° and the dip is 15°ESE. The dimensions of the subfault elements are 14 km in the strike direction and 10 km in the dip direction. The rupture surface is approximately 70 km along strike and 20 km along downdip. The seismic moment release based upon this plane is 7.1e+27 dyne.cm. DISCLAIMER Base map data, such as place names and political boundaries, are the best available but may not be current or may contain inaccuracies and therefore should not be regarded as having official signifiance. Map updated by U.S. Geological Survey National Earthquake Information Center 18 April 2016 http://earthquake.usgs.gov/ Map not approved for release by Director USGS M7.8 Coastal Ecuador Earthquake of 16 April 2016 16 April 2016 23:58:37 UTC 0.371° N., 79.94° W. Depth 19.2 km Mw = 7.8 (USGS) COCOS PLATE Finite Fault Model SOUTH AMERICA PLATE CARIBBEAN PLATE

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Page 1: U.S. GEOLOGICAL SURVEY M7.8 Coastal Ecuador Earthquake of ...app.sni.gob.ec/.../RESUMEN_TERREMOTO_ECUADOR_USGS.pdf · d et mina o;Bu l .Ss c A ,v 8 p 72- 43 EARTHQUAKE SUMMARY MAP

U.S. DEPARTMENT OF THE INTERIORU.S. GEOLOGICAL SURVEY

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Manizales

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Guayaquil

PacificOcean

Colombia

Ecuador

Peru

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CaribbeanSea

AtlanticOcean

PacificOcean

68 mm/yr78 mm/yr

74 mm/yr

19 mm/yr

20 mm/yr20 mm/yr

65 mm/yr

58 mm/yr

71 mm/yr

68 mm/yr

61 mm/yr

65°

65°

75°

75°

85°

85°

95°

95°

15° 15°

5° 5°

5° 5°

15° 15°

M7.8 Coastal Ecuador Earthquake of 16 April 2016

0 250 500125Kilom e te rs

65°

65°

75°

75°

85°

85°

95°

95°

5° 5°

5° 5°

0 500 1,000 1,500250Kilom e te rs

Prepared in cooperation with the Global Seismographic Network

Tectonic Setting

Seismic Hazard

Epicentral Region

TECTON IC SUMMARYThe April 16, 2016 M 7.8 e arthqua ke , offs hore of the we s t coa s t of northe rn Ecua d or, occurre d a s the re s ult of s ha llow thrus t fa ulting on or ne a r the pla te b ound a ry b e twe e n the N a zca a nd Pa cific pla te s . At theloca tion of the e a rthqua ke , the N a zca pla te sub d ucts e a s tward b e ne a th the South Am erica pla te a t a ve locity of 61 m m /yr. The loca tion a nd m e cha nis m of the e a rthqua ke a re cons is te nt with s lip on the prim a ry pla teb ound a ry inte rfa ce , or m e g a thrus t, b e twe e n the s e two m a jor pla te s . Sub d uction a long the Ecua d or Tre nch to the we s t of Ecua d or, a nd the Peru-Chile Tre nch further s outh, ha s le d to uplift of the And e s m ounta inra ng e a nd ha s prod uce d s om e of the larg e s t e a rthqua ke s in the world , includ ing the larg e s t e a rthqua ke on re cord , the 1960 M 9.5 e arthqua ke in s outhe rn Chile .While com m only plotte d a s points on m a ps , e a rthqua ke s of this s ize are m ore a ppropria te ly d e s crib e d a s s lip ove r a la rg e r fa ult a re a . Eve nts of the s ize of the April 16, 2016 e arthqua ke a re typica lly a b out 160x60 kmin s ize (le ng th x wid th).Ecua d or ha s a his tory of larg e sub d uction zone re la te d e a rthqua ke s . Se ve n m a g nitud e 7 or g re a te r e a rthqua ke s ha ve occurre d within 250 km of this e ve nt s ince 1900. On Ma y 14th, 1942, a M 7.8 e arthqua keoccurre d 43 km s outh of this April 16th, 2016 e ve nt. On Ja nuary 31s t, 1906 a M 8.3 e arthqua ke (re porte d ly a s la rg e a s M 8.8 in s om e s ource s ) nucle a te d on the s ub d uction zone inte rfa ce 90 km to the northe a s t of theApril 2016 e ve nt, a nd rupture d ove r a le ng th of a pproxim a te ly 400-500 km , re s ulting in a d a m a g ing ts una m i tha t ca us e d in the re g ion of 500-1,500 fa ta litie s . The April 2016 e arthqua ke is a t the s outhe rn e nd of thea pproxim a te rupture are a of the 1906 e ve nt. A s ha llow, upper crus ta l M 7.2 e arthqua ke 240 km e a s t of the April 2016 e ve nt on March 6th, 1987 re s ulte d in a pproxim a te ly 1,000 fa ta litie s .

EXPLANATIONMain Shock

_̂Aftershocks!(

Earthquake Magnitude( 5.5 - 6.5( 6.5 - 7.0

( 7.0 - 7.5

( 7.5 - 8.0

( > 8.0

Earthquake Depth (km)!( 0 - 69

!( 70 - 299

!( ≥ 300

Finite Fault ModelSlip (mm)

Ô < 50

Ô 50 - 150

Ô 150 - 250

Ô 250 - 270

Ô 270 - 340

Ô > 340

Plate Boundaries# Sub d uction

Tra ns form

Dive rg e nt

Othe rs

Seismic hazard is expressed as peakground acceleration (PGA) on firmrock, in meters/sec², expected to beexceeded in a 50-yr period with aprobability of 10 percent.

EXPLANATIONMa g ≥ 7.0 !( 0 - 69 km!( 70 - 299!( 300 - 600

Plate Boundaries# Sub d uction

Tra ns formDive rg e ntOthe rs

0 500 1,000 1,500250Kilom e te rs

Pe a k Ground Acce le ra tion in m /s e c**2

.2 .4 .8 1.6 2.4 3.2 4.0 4.8

Epicentral Region

Epicentral Region

DATA SOURCESEARTHQUAKES AND SEISMIC HAZARD USGS, National Earthquake Information Center NOAA, National Geophysical Data Center IASPEI, Centennial Catalog (1900 - 1999) and extensions (Engdahl and Villaseñor, 2002)EHB catalog (Engdahl et al., 1998)HDF (unpublished earthquake catalog, Engdahl, 2003)Global Seismic Hazard Assessment ProgramVolcanoes of the World (Siebert and Simkin, 2002)PLATE TECTONICS AND FAULT MODELPB2002 (Bird, 2003)Ji, C., D.J. Wald, and D.V. Helmberger, Source description of the 1999 Hector Mine, California earthquake; Part I: Waveletdomain inversion theory and resolution analysis, Bull. Seism. Soc. Am., Vol 92, No. 4. pp. 1192-1207, 2002.DeMets, C., Gordon, R.G., Argus, D.F., 2010.Geologically current plate motions, Geophys. J. Int. 181, 1-80.

BASE MAPNIMA and ESRI, Digital Chart of the WorldUSGS, EROS Data CenterNOAA GEBCO and GLOBE Elevation Models

REFERENCESBird, P., 2003, An updated digital model of plate boundaries: Geochem. Geophys. Geosyst., v. 4, no. 3, pp. 1027-80.

Engdahl, E.R., and Villasenor, A., 2002, Global Seismicity: 1900-1999, chap. 41 of Lee, W.H.K., and others, eds., International Earthquake and Engineering Seismology, Part A: New York, N.Y.,Elsevier Academic Press, 932 p.Engdahl, E.R., Van der Hilst, R.D., and Buland, R.P.,1998, Global teleseismic earthquake relocation with improved travel times and procedures for depth determination;Bull. Seism. Soc. Amer., v. 88, p. 722-743.

EARTHQUAKE SUMMARY MAP

NAZCAPLATE

PAGER

Dis tribution of the a m plitud e a nd d ire ction of s lip for sub fa ult e le m e nts of the fa ult rupture m od e l a re d e te rm ine dfrom the inve rs ion of te le s e is m ic bod y wa ve form s a nd long pe riod s urfa ce wa ve s . Arrows ind ica te the a m plitud ea nd d ire ction of s lip (of the ha ng ing wa ll with re s pe ct to the foot wa ll); the s lip is a ls o colore d by m a g nitud e . Thevie w of the rupture pla ne is from a b ove . The s trike of the fa ult rupture pla ne is 29° a nd the d ip is 15°ESE. Thed im e ns ions of the s ub fa ult e le m e nts a re 14 km in the s trike d ire ction a nd 10 km in the d ip d ire ction. The rupturesurfa ce is a pproxim a te ly 70 km a long s trike a nd 20 km a long d ownd ip. The s e is m ic m om e nt re le a s e b a s e dupon this pla ne is 7.1e+27 d yne .cm .

DISCLAIMER

Base map data, such as place names and political boundaries, are the best available but may not be current or may contain inaccuracies and therefore should not be regarded as having official signifiance.Map updated by U.S. Geological Survey National Earthquake Information Center 18 April 2016http://earthquake.usgs.gov/ Map not approved for release by Director USGS

M7.8 Coastal Ecuador Earthquake of 16 April 2016 16 April 2016 23:58:37 UTC 0.371° N., 79.94° W.Depth 19.2 kmMw = 7.8 (USGS)

COCOSPLATE

Finite Fault Model

SOUTH AMERICA PLATE

CARIBBEAN PLATE