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Sierra Maestra Range

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Eastern Cuba and isoseismals scheme and the epicenter of the August 20, 1852 earthquake. (A) Epicenter (black circle); intensity 5–8 degrees (MSK); localities (B: Bayamo, BA: Baracoa, BAC: Baconao, BT: Baitiquirí, C: Camagüey, CA: Caney, CAS: Cascorro, CC: Cabo Cruz, CO: El Cobre, CR: Cauto River, G: Guantánamo, GG: Guacanayabo Gulf, GI: Gibara, GP: Gran Piedra Range, H: Holguín, J: Jiguaní, JO: Jobabo, M: Manzanillo, MA: Mayarí, N: Niquero, NV: Nuevitas, P: Pilón, PPA: Puerto Padre, PM: Punta de Maisí, SC: Santiago de Cuba, SL. San Luis, SMR: Sierra Maestra Range, ST: Sagua de Tánamo). (B) Faults (BF: Baconao, CNF: Cauto-Nipe, OF: Oriente); localities (1: Sierra Maestra Range, 2: Cauto basin, 3: NW Mountains, 4: Nipe–Cristal–Baracoa Mountains, 5: Cabo Cruz area). (C) Panoramic view of Santiago de Cuba and its surroundings (AG: Aguadores, CJ: Cojímar, CO: El Cobre, CT: Contramaestre, D: Daiquiri, EC: El Caney, EM: El Morro, ES: El Sardinero, JU: Juraguá, LG: Las Guásimas, MV: Mar Verde, PA: Palma Soriano, SCB: Santiago de Cuba Bay, SCC: Santiago de Cuba City, SI: Sigua, SL: San Luis, SO: La Socapa); epicenter of 1852.
Published: 01 November 2010
: Cauto River, G: Guantánamo, GG: Guacanayabo Gulf, GI: Gibara, GP: Gran Piedra Range, H: Holguín, J: Jiguaní, JO: Jobabo, M: Manzanillo, MA: Mayarí, N: Niquero, NV: Nuevitas, P: Pilón, PPA: Puerto Padre, PM: Punta de Maisí, SC: Santiago de Cuba, SL. San Luis, SMR: Sierra Maestra Range, ST: Sagua de
Image
Santiago de Cuba area (SANTO DOMINGO 066 (–AI denomination–)). 1: Cathedral, 2: Nuestra Señora del Carmen Church, 3: Convent of San Francisco, 4: Mayor, 5: El Morro Castle, 6: Batteries of the La Plataforma and La Punta, 7: Battery of La Estrella, 8: Aguadores Fort, 9: coastal segment of the bay, 10: Sierra Maestra Range, 11: Mar Verde Fort, SC Bay: Santiago de Cuba Bay, SCC: Santiago de Cuba City.
Published: 01 November 2010
of the bay, 10: Sierra Maestra Range, 11: Mar Verde Fort, SC Bay: Santiago de Cuba Bay, SCC: Santiago de Cuba City.
Image
Cuban megablock according to Cotilla et al. (1991). (a) Heavy black line, faults: CNF, Cauto-Nipe; NCF, Nortecubana; OF, Oriente; SCF, Surcubana; Neotectonic Unit: OC, Western; OR, Eastern; crust type: 1, postorogenic complex; 2, orogenic complex; 3, volcanic arc complex; localities: C, Camagüey; CS, Cabo de San Antonio; LH, La Habana; PM, Punta de Maisí. (b) Santiago de Cuba area. Heavy black line, Oriente Fault (OF); localities: BL, Baconao lagoon; DB, Dos Bocas; EC, El Cobre; GU, Güira; JB, Jíbacoa; LS, La Socapa; MC, Morro Castle; MV, Mar Verde; S, Sardinero; SA, Salado; SC, Santiago de Cuba City; SCB, Santiago de Cuba Bay. Other structures: GPR, Gran Piedra Range. (c) Eastern Cuba. Localities: B, Baitiquirí; C, Camgüey; G, Guantánamo; H, Holguín; M, Mayarí; SC, Santiago de Cuba City; SMR, Sierra Maestra Range. Other structures: OF, Oriente Fault; OT, Oriente trough.
Published: 01 February 2010
; SC, Santiago de Cuba City; SCB, Santiago de Cuba Bay. Other structures: GPR, Gran Piedra Range. ( c ) Eastern Cuba. Localities: B, Baitiquirí; C, Camgüey; G, Guantánamo; H, Holguín; M, Mayarí; SC, Santiago de Cuba City; SMR, Sierra Maestra Range. Other structures: OF, Oriente Fault; OT, Oriente
Journal Article
Published: 01 November 2010
Russ. Geol. Geophys. (2010) 51 (11): 1227–1246.
...: Cauto River, G: Guantánamo, GG: Guacanayabo Gulf, GI: Gibara, GP: Gran Piedra Range, H: Holguín, J: Jiguaní, JO: Jobabo, M: Manzanillo, MA: Mayarí, N: Niquero, NV: Nuevitas, P: Pilón, PPA: Puerto Padre, PM: Punta de Maisí, SC: Santiago de Cuba, SL. San Luis, SMR: Sierra Maestra Range, ST: Sagua de...
FIGURES | View All (8)
Journal Article
Published: 01 June 2007
Russ. Geol. Geophys. (2007) 48 (6): 505–522.
... by a more than 7 km deep (Bartlett or Oriente) and in the emerged relief by an approximately 2 km high range, the Sierra Maestra. Therefore, the break is approximately 10 km. There is a steep but very irregular slope on the southern Cuban margin. The morphologic expression is a clear indicator...
FIGURES | View All (12)
Journal Article
Published: 01 December 1922
Bulletin of the Seismological Society of America (1922) 12 (4): 199–219.
..., thus separating the two islands. According to this hypothesis the Southern Range of Haiti extending~ along the Tiburon Peninstfla would be a horst lying between the two branches of a fault system. The Cayman Islands-Sierra Maestra-North Haiti fault zone .ex- tends along the north side of the Bartlett...
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1932
AAPG Bulletin (1932) 16 (6): 533–555.
... to belong to this series. Fragments of these limestones ranging up to a kilometer in length are included within the serpentine areas of Camaguey and western Oriente provinces. Cretaceous pyroclastics and limestones are reported on the northern flank of the Sierra Maestra in Oriente Province. Also...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1969
AAPG Bulletin (1969) 53 (12): 2494–2500.
... Jurassic intrusion; Meyerhoff and Hatten (1968) believe the Tres Guanos to be Paleozoic. Localities 7–9 ( Table 1 ; Fig. 1 ) are in the Sierra Maestra west and east of Santiago de Cuba, along the south coast of Oriente Province. The 46–58 m.y. dates show that quartz dioritic rocks intruded...
FIGURES
Journal Article
Published: 01 September 1912
Bulletin of the Seismological Society of America (1912) 2 (3): 161–180.
... between the two great land-masses of the southern range: La Selle and La Hotte. The fact that an earth- quake "transgresses," in the etymological sense of the word, has been seen equally well in the earthquake of 1842, which shook the north of the Grande Hilera of Haiti and the south of the Sierra Maestra...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1975
AAPG Bulletin (1975) 59 (5): 838–855.
... and west. In the Sierra Maestra of southern Oriente Province, the sequence of volcanic rocks is estimated to reach a thickness of 6,000 m. Intermediate and acidic intrusives are characteristic—diorites and granodiorites—forming batholiths in Camaguey and northern Oriente ( Nagy, 1973 ), as well as small...
FIGURES | View All (6)
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1949
AAPG Bulletin (1949) 33 (8): 1319–1335.
..., indicating a flank of an uplift whose axis probably passes through the Coxcomb Mountains and perhaps continues through the Cayman Islands toward the Sierra Maestra of southeast Cuba. The Chiapas massif is south of the geosynclinal folds and forms the southernmost blocks of the hinterland...
FIGURES
Journal Article
Published: 01 November 2009
The Journal of Geology (2009) 117 (6): 685–692.
... , Y. ; Neubauer , F. ; Kröner , A. ; Wan , Y. S. ; Liu , D. Y. ; García-Delgado , D. E. ; and Handler , R. 2004 . Geochemistry and early Paleogene SHRIMP zircon ages of island arc granitoids of the Sierra Maestra, southeastern Cuba . Chem. Geol. 213 : 307 – 324...
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Journal Article
Published: 01 February 2010
Russ. Geol. Geophys. (2010) 51 (2): 228–236.
...; SC, Santiago de Cuba City; SCB, Santiago de Cuba Bay. Other structures: GPR, Gran Piedra Range. ( c ) Eastern Cuba. Localities: B, Baitiquirí; C, Camgüey; G, Guantánamo; H, Holguín; M, Mayarí; SC, Santiago de Cuba City; SMR, Sierra Maestra Range. Other structures: OF, Oriente Fault; OT, Oriente...
FIGURES
Journal Article
Published: 01 November 2011
The Journal of Geology (2011) 119 (6): 619–640.
... ; Iturralde-Vinent et al. 2006 ; Proenza et al. 2006 ), and a tholeiitic Paleogene complex (Sierra Maestra), which developed only in eastern Cuba (fig. 1 b , 1 c ; 60.5 ± 2.2 to 46.9 ± 0.1 Ma; Kysar et al. 1998 ; Rojas-Agramonte et al. 2004 ). In addition, Kerr et al. ( 1999...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1954
AAPG Bulletin (1954) 38 (5): 707–773.
... trending provinces, namely, the volcanic province and the Sierra del Sur. The volcanic province is very rugged with volcanic peaks rising to 18,240 feet. The Sierra del Sur on the south consists, as far as known, of subparallel east-west ranges. Its rocks are Paleozoic and Mesozoic sediments, with Mesozoic...
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Journal Article
Published: 01 September 2004
The Journal of Geology (2004) 112 (5): 521–542.
... ending formation of the Cretaceous volcanic arc. Although the three La Sierra samples from Las Margaritas show a relatively large range of ages for biotite and K-feldspar, ages for K-feldspar are not systematically lower than those for biotite. In view of the very different closure temperatures...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1943
AAPG Bulletin (1943) 27 (11): 1407–1533.
..., and in the Sierra Madre Oriental from the region of Saltillo southward to southern Nuevo León and southwestern Tamaulipas. Its thickness ranges from about 200 to more than 1,400 feet. The La Caja formation is the offshore equivalent of the La Casita formation and consists of thin-bedded limestone, marl, and shale...
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Journal Article
Journal: Geosphere
Published: 21 November 2019
Geosphere (2020) 16 (1): 210–228.
.... , Hejl , E. , Handler , R. , and García-Delgado , D.E. , 2006 , Geology, age and tectonic evolution of the Sierra Maestra Mountains, southeastern Cuba : Geologica Acta , v. 4 , p. 123 – 150 , https://doi.org/10.1344/105.000000361 . Rossello , E.A. , Rey , A. , and Ramírez...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1960
AAPG Bulletin (1960) 44 (8): 1273–1315.
... into a series of east-west-trending mountain ranges. Principal among these are: Sierra de Los Cuchumatanes, Sierra de Chuacus, Sierra de Las Minas, Sierra de Santa Cruz, and the Montana del Mico. The location of these ranges is shown in Figure 2 . This belt of mountain ranges parallels the volcanic Cordillera...
FIGURES | View All (20)
Journal Article
Published: 01 June 1920
Bulletin of the Seismological Society of America (1920) 10 (2): 55–89.
... 8,~7a meters below the higher peaks of the Sierra Maestra in southern Cuba and of the Blue Mountains in Jamaica. The six deepest places located by soundings (all over 3000 fathoms or 5486 meters) are situated close to the foot of the inclosing scarps rather than near the center of the trench...