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Seismicity of the Earth 1900–2010

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Seismicity of the Earth 1900–2010 U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY OPEN-FILE REPORT 2010–1083-A Revised September, 2011 Seismicity of the Earth 1900–2010 TECTONIC SUMMARY Caribbean Plate and Vicinity Extensive diversity of tectonic regimes characterizes the perimeter of the Caribbean plate, involving no fewer than four major adjacent plates (North America, South America, Nazca, and Cocos). Inclined zones of deep earthquakes (Wadati-Benioff zones), deep ocean Compiled by Harley M. Benz,1 Arthur C. Tarr,1 Gavin P. Hayes,1 Antonio Villaseñor,2 Kevin P. Furlong,2 Richard L. Dart,1 and Susan Rhea1 trenches, and arcs of volcanoes clearly indicate subduction of oceanic lithosphere along the Central American and Atlantic Ocean margins of the Caribbean plate, while shallow seismicity and focal mechanisms of major shocks in Guatemala, northern Venezuela, 2011 and the Cayman Ridge and Cayman Trench indicate transform fault and pull-apart basin tectonics. 1U.S. Geological Survey The depth profile panels on this map portray earthquakes that extend from the Middle America Trench axis in the west to depths as 2Institute of Earth Sciences, CSIC, Barcelona, Spain 3 great as 300 km beneath Guatemala, and from the Lesser Antilles Trench axis in the east to depths of approximately 200 km beneath Department of Geosciences, Pennsylvania State University, State College, PA 16802 USA 95° 90° 85° 80° 75° 70° 65° 60° Guadeloupe and the northeast Caribbean. In contrast, seismicity along the segments of the Caribbean plate margins from Guatemala gh B to Hispaniola and from Trinidad to western Venezuela is indicative of transform fault tectonics. Mexico Basin Bahama BankGreat Exuma a h GG -300 -200 -100 0 ' A r c a h . d Long I. m Gulf of Mexico e C a BAHAMAS Along the northern margin of the Caribbean plate, the North America plate moves west, relative to the Caribbean plate, at approximately Havana a m I s TRENCH AXIS a g Crooked I. l a 20 mm/yr, resulting in major transcurrent faults and troughs. Farther east, the North America plate subducts beneath the Caribbean plate AA'0 100 200 300 400 ü e n d 0 y s resulting in surface expression of the deep Puerto Rico Trench and a zone of intermediate focus earthquakes in the subducted slab. Campeche Bank Mayaguana I. ATLANTIC OCEAN TRENCH AXIS Cayo Romano Acklins I. 0 Caicos Is. (U.K.) TURKS AND -100 The plate boundary curves around Puerto Rico and the northern Lesser Antilles where the plate motion vector of the Caribbean plate Isla de la Caicos CAICOS IS. (U.K.) relative to the North and South America plates is less oblique, resulting in active island-arc tectonics. The North and South America Juventud Bank Turks Island plates subduct beneath the Caribbean plate along the Lesser Antilles Trench at rates of about 20 mm/yr; consequently, there are both -100 Ja CUBA Grand Inagua PROFILE G rd -200 intermediate focus earthquakes within the subducted South America plate and a chain of active volcanoes along the island arc. i Island Merida ne s d e Silver la Rein Bank The southern Caribbean plate boundary along with the South America plate strikes east-west across Trinidad and western Venezuela Isla Cozumel a Hispaniola Trough -200 Navidad G' and is characterized by major strike-slip faults and shallow seismicity, resulting from relative plate motion of about 20 mm/yr. Further Santiago De Cuba R 20° Bank P U E R T O I C O T R E N C H 20° PROFILE A 1946 to the west, a broad zone of convergent deformation trends southwest across western Venezuela and central Columbia. Plate CAYMAN IS. boundaries are not well defined across northern South America, but there is a transition from Caribbean/South America convergence Bay of (U.K.) H FF' -300 N C -300 -200 -100 0 Veracruz Grand Cayman I. E 1943 in the east to Nazca/South America convergence in the west, described in more detail below. The transition zone is characterized by Campeche R Île de la HAITI 1946 BRITISH T G DOMINICAN 50 VIRGIN h R Gonâve r o u g high seismic hazard. N HispaniolaREPUBLIC ISLANDS (U.K.) T TRENCH AXIS A E r o MEXICO M A Port-au-Prince Santo Domingo e 0 Yucatan Basin Cayman Ridge r Y T 100 b St. Martin The Nazca-Caribbean plate boundary offshore of Columbia is characterized by convergence (Nazca plate subducting under South A E mAnguilla (U.K.) PUERTO RICO (U.S.) o (France & Neth. Antilles) Villahermosa C JAMAICA R Mona Trough America plate) at about 65 mm/yr. The January 6, 1906 Mw = 8.5 megathrust subduction earthquake occurred on a shallow-dipping Kingston Mona I. 200 U.S. VIRGINS Vieques (U.S.) ISLANDS (U.S.) -100 interface of this plate boundary segment. The 1906 earthquake occurred in the Colombia-Ecuador region, with a seismic moment A' Barbuda A N St. Croix ST. KITT'S (Mo; equivalent to radiated energy) of 6×10 Exp 28 dyne-cm (Okal, 1992), and a moment magnitude (Mw) of 8.5 (Tarr and others, BELIZE T AND NEVIS ANTIGUA AND 200 I M Yuma Trough H St. Kitt's Turneffe Is. L U E R T O S T R O U G BARBUDA Rosalind Bank L L L 2010). The nucleation point of this earthquake is indicated on the map (rupture area is from Kanamori and McNally, 1982). P E ee Nevis PROFILE F e d E S w Antigua r o Ban k G S E a -200 Tuxtla Gutierrez S R r d Montserrat (U.K.) Is la F' Along the western coast of Central America, the Cocos plate subducts beneath the Caribbean plate at rates of 72–81 mm/yr, resulting Isla de la Gulf of e n Guadeloupe g d Roatán s L 1902 d (France) in a relatively high seismic hazard and a chain of numerous active volcanoes; here intermediate-focus earthquakes occur within the Honduras i Alice Kingston Bank E R Shoal subducted Cocos plate to depths of nearly 300 km. Serranilla s A Marie-Galante S B' Beata Ridge o Bank y N S a San Pedro Sula g Lightning Bank T E 1976 a DATA SOURCES B' p DominicaI DOMINICA R Caribbean Sea a L GUATEMALA P F Aves Ridge L A n i 15° s 15° The earthquakes portrayed on the main map and the depth profiles are taken from two sources: (a) the Centennial earthquake catalog E Martinique N . a W Guatemala City B Z o S (France) T o (Engdahl and Villaseñor, 2002) and annual supplements for the interval 1900–2007, where the magnitude floor is 5.5 globally, and (b) e 1950 HONDURAS C' d g Cayos Miskitos a w I d i d a L a catalog of earthquakes having high-quality depth determinations for the period 1964–2002 and a magnitude range of 5.0≥M≤5.4 a M Tegucigalpa Venezuela Basin R r 1902 d n L A a I I ST. LUCIA D 1942 EL SALVADOR r r s (Engdahl, personal commun., 2009.) Sue Ridge e la E G D n n St. Lucia Tehauntepec Ridge i r ds L e S a n i E San Salvador g M s d i A Isla de Providencia a The nucleation points of great earthquakes (M≥8.3) are designated with a label showing the year of occurrence. Their rupture areas T ST. VINCENT AND R M 2001 B BARBADOS E R THE GRENADINES St. Vincent Barbados are shown as pale reddish polygons. Major earthquakes (7.5≥M≤8.2) are labeled with the year of occurrence, while earthquakes R s o NETHERLANDS o I g E C d E a a A NICARAGUA Aruba (Neth.) ANTILLES b (8.0≥M≤8.2) are labeled with the year of occurrence and also denoted by a white outline (Tarr and others, 2010). N b Islas o Isla de San Andres r T T R The Grenadines a Golfo de Fonseca 300 Los Roques C E B B N Managua Bonaire (Venez.) GRENADA C I. del Maiz Grande Isla Grenada H The Seismic Hazard and Relative Plate Motion map displays the generalized seismic hazard of the region (Giardini and others, 1999) and H 1992 Curaçao Lago de Orchilla Isla Blanquilla representative relative plate motion vectors of the Caribbean plate relative to the adjacent North and South America plates using the Nicaragua Colombian Basin (Venez.) (Venez.) 100 Golfo de NUVEL–1A model (DeMets and others, 1994, 2000) and updates (Dixon and others, 1998; Weber and others, 2001). B 0 100 200 300 400 B' 50 Isla La Tortuga Venezuela 1900 Isla de Tobago (Venez.) Margarita C Barranquilla (Venez.) TRINIDAD AND Pre-instrumental seismicity for the Caribbean basin was obtained from the NOAA National Geophysical Data Center (2010) database TRENCH AXIS TOBAGO Maracaibo of significant earthquakes; locations are approximate, based on macro-seismic reports and field investigations. We selected 0 COSTA RICA D' Clark Cartagena Caracas earthquakes with associated reports of moderate to major damage, 10 or more deaths, an estimated magnitude of 7.5 or greater (if Basin Valencia E' Barquisimeto Maracay known), Modified Mercalli Intensities X, or tsunami generation. 10° 1991 Lago de Trinidad 10° E -500-400 -300 -200 -100 0 E' -100 Guardian Seamount Maracaibo Volcan Bank Base map data sources include GEBCO 2008, Volcanoes of the World dataset (Siebert and Simkin, 2002), plate boundaries (Bird, Golfo de Los Panama 2003), Digital Chart of the World (1992), and Environmental Sciences Research Institute (ESRI, 2002). Slab contours are from Hayes and Wald Fisher 1983 Mosquitos TRENCH AXIS 0 -200 Seamount Bahia de Panamá (2010).
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