U.S Geological Survey Open-File Report 98-38 Geology, Geochemistry, Geophysics, Mineral Occurrences and Mineral Resource Assessm
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1 Climatology of Tropical Cyclone Rainfall Over
CLIMATOLOGY OF TROPICAL CYCLONE RAINFALL OVER PUERTO RICO: PROCESSES, PATTERNS AND IMPACTS By JOSÉ JAVIER HERNÁNDEZ AYALA A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 2016 1 © 2016 José Javier Hernández Ayala 2 To my beloved Puerto Rico, its atmosphere, environment and people 3 ACKNOWLEDGMENTS The main ideas behind the development of this dissertation came from multiple experiences with tropical cyclones while living in Puerto Rico. Those life experiences motivated me to explore the climate of the tropics, with special attention to the rainfall associated with those extreme events and their role in Puerto Rico’s physical geography. The research conducted in this dissertation was possible from support of Dr. Corene Matyas, Associate Professor and Graduate Coordinator at the Department of Geography at the University of Florida. Her magnificent mentoring and continuous support enable me to invest the necessary effort and time to complete this dissertation. I am truly grateful for her exceptional role as my committee chair. I want to thank Dr. Peter Waylen for his continuous support and all of the inspiring conversations we’ve had about research and life in general that gave me even more strength to continue in this journey towards the PhD. I thank Dr. Timothy Fik for sharing his expertise in quantitative methods through two great courses and for inspiring me to aspire to more in life. Thanks to Dr. Zhong-Ren Peng for being my external committee member and teaching me more about the human dimension of climate related phenomena. -
Tectonics and Sedimentation in Foreland Basins: Results from the Integrated Basin Studies Project
Downloaded from http://sp.lyellcollection.org/ by guest on September 30, 2021 Tectonics and sedimentation in foreland basins: results from the Integrated Basin Studies project ALAIN MASCLE 1 & CAI PUIGDEFABREGAS 2,3 IIFP School, 228-232 avenue Napoldon Bonaparte, 92852 Rueil-Malmaison Cedex, France (e-mail: [email protected]) 2Norsk Hydro Research Centre, Bergen, Norway. 3Institut de Ciences de la Terra, (?SIC, Barcelona, Spain. Why foreland basins? to a better understanding of some basic interact- ing tectonic, sedimentary and hydrologic pro- Over the last ten years or so, since the Fribourg cesses (More & Vrolijk 1992; Touret & van meeting in 1985 (Homewood et al. 1986), the Hinte 1992). Additional data have also been attention given by sedimentologists and struc- obtained through the development of analogue tural geologists to the geology of foreland basins and numerical models (Larroque et al. 1992; has been growing continuously, parallel to the Zoetemeijer 1993). The physical parameters increase of co-operative links between scientists controlling the forward propagation of d6colle- from the two disciplines. A number of reasons ments and thrusts (fluid pressure, roughness, lie behind this development. Attempting to sediment thickness, etc.) have been determined understand the growth of an orogen without and tested. The relationships between rapidly paying due attention to the stratigraphic record subsiding piggyback basins and growing ramp of the derived sediments would be unrealistic. It anticlines have also been imaged, although the would, moreover, be equally unrealistic to con- lack of deep-sea well control still prevents accu- struct restored sections across the chain without rate sedimentological studies. More significant considering the constraints imposed by the has been the progress in our understanding of basin-fill architecture, or to describe the basin- the role of fluids and pore pressure in the fill evolution disregarding the development of development of thrust belts. -
Resumen Ejecutivo
U.S. Fish and Wildlife Service BORRADOR DEL PLAN ABARCADOR DE CONSERVACIÓN BORRADOR DELPLANABARCADORDECONSERVACIÓN DELAGUNACARTAGENA REFUGIO NACIONALDEVIDASILVESTRE Susan Silander, Supervisora de los Refugios de Vida Silvestre del Caribe Oscar A. Díaz-Marrero, Administrador del Refugio Refugio Nacional de Pesca y Vida Silvestre de Laguna Cartagena P.O. Box 510 Boquerón, PR 00622 REFUGIOREFUGIO NACIONALNACIONAL DEDE VIDAVIDA Teléfono: (787) 851-7258 SILVESTRESILVESTRE Fax (787) 255-6725 DEDE LAGUNALAGUNA CARTAGENACARTAGENA E-mail [email protected] BORRADORBORRADOR DELDEL PLANPLAN ABARCADORABARCADOR Servicio Federal de Pesca y Vida Silvestre 1-800-344-WILD DEDE CONSERVACIÓNCONSERVACIÓN http:www.fws.gov julio 2011 Photo provided by Jim Abernethy’s Scuba Adventures Front Cover Photo Credits: Background/open water - David Bocanegra/USFWS Yellow crown night heron - Bryant Marcial/USFWS Whistling duck - Bryant Marcial/USFWS Orange bishop bird - Bryant Marcial/USFWS Photo blind structure - David Bocanegra/USFWS Observation tower - David Bocanegra/USFWS Common moorhen - Bryant Marcial/USFWS White-cheeked Pintail - Bryant Marcial/USFWS Whistling duck - Bryant Marcial/USFWS Refuge sign - David Bocanegra/USFWS Comprehensive Conservation Plans provide long-term guidance for management decisions; set forth goals, objectives, and strategies needed to accomplish refuge purposes; and identify the Fish and Wildlife Service’s best estimate of future needs. These plans detail program planning levels that are sometimes substantially above current budget allocations -
French Massif Armoricain
The Léon Domain (French Massif Armoricain): a westward extension of the Mid-German Crystalline Rise? Structural and geochronological insights Michel Faure, Claire Sommers, Jérémie Melleton, Alain Cocherie, Olivier Lautout To cite this version: Michel Faure, Claire Sommers, Jérémie Melleton, Alain Cocherie, Olivier Lautout. The Léon Domain (French Massif Armoricain): a westward extension of the Mid-German Crystalline Rise? Structural and geochronological insights. International Journal of Earth Sciences, Springer Verlag, 2010, 99 (1), pp.65-81. 10.1007/s00531-008-0360-x. insu-00352053 HAL Id: insu-00352053 https://hal-insu.archives-ouvertes.fr/insu-00352053 Submitted on 12 Jan 2009 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. The Léon Domain (French Massif Armoricain): a westward extension of the Mid-German Crystalline Rise? Structural and geochronological insights Michel Faure1 , Claire Sommers1, Jérémie Melleton1, 2, Alain Cocherie2 and Olivier Lautout1 (1) ISTO Campus Géosciences, Orléans University, 1A Rue de la Férollerie, 45071 Orléans Cedex 2, France (2) BRGM, Av. Claude-Guillemin, 45060 Orléans Cedex 2, France Abstract The Léon Domain in the NW part of the French Massif Armoricain is a stack of synmetamorphic nappes displaced from south to north in ductile conditions. -
Sitios Arqueológicos De Ponce
Sitios Arqueológicos de Ponce RESUMEN ARQUEOLÓGICO DEL MUNICIPIO DE PONCE La Perla del Sur o Ciudad Señorial, como popularmente se le conoce a Ponce, tiene un área de aproximadamente 115 kilómetros cuadrados. Colinda por el oeste con Peñuelas, por el este con Juana Díaz, al noroeste con Adjuntas y Utuado, y al norte con Jayuya. Pertenece al Llano Costanero del Sur y su norte a la Cordillera Central. Ponce cuenta con treinta y un barrios, de los cuales doce componen su zona urbana: Canas Urbano, Machuelo Abajo, Magueyes Urbano, Playa, Portugués Urbano, San Antón, Primero, Segundo, Tercero, Cuarto, Quinto y Sexto, estos últimos seis barrios son parte del casco histórico de Ponce. Por esta zona urbana corren los ríos Bucaná, Portugués, Canas, Pastillo y Matilde. En su zona rural, los barrios que la componen son: Anón, Bucaná, Canas, Capitanejo, Cerrillos, Coto Laurel, Guaraguao, Machuelo Arriba, Magueyes, Maragüez, Marueño, Monte Llanos, Portugués, Quebrada Limón, Real, Sabanetas, San Patricio, Tibes y Vallas. Ponce cuenta con un rico ajuar arquitectónico, que se debe en parte al asentamiento de extranjeros en la época en que se formaba la ciudad y la influencia que aportaron a la construcción de las estructuras del casco urbano. Su arquitectura junto con los yacimientos arqueológicos que se han descubierto en el municipio, son parte del Inventario de Recursos Culturales de Ponce. Esta arquitectura se puede apreciar en las casas que fueron parte de personajes importantes de la historia de Ponce como la Casa Paoli (PO-180), Casa Salazar (PO-182) y Casa Rosaly (PO-183), entre otras. Se puede ver también en las escuelas construidas a principios del siglo XX: Ponce High School (PO-128), Escuela McKinley (PO-131), José Celso Barbosa (PO-129) y la escuela Federico Degetau (PO-130), en sus iglesias, la Iglesia Metodista Unida (PO-126) y la Catedral Nuestra Señora de Guadalupe (PO-127) construida en el siglo XIX. -
Puerto Rico, Colonialism In
University at Albany, State University of New York Scholars Archive Latin American, Caribbean, and U.S. Latino Latin American, Caribbean, and U.S. Latino Studies Faculty Scholarship Studies 2005 Puerto Rico, Colonialism In Pedro Caban University at Albany, State Univeristy of New York, [email protected] Follow this and additional works at: https://scholarsarchive.library.albany.edu/lacs_fac_scholar Part of the Latin American Studies Commons Recommended Citation Caban, Pedro, "Puerto Rico, Colonialism In" (2005). Latin American, Caribbean, and U.S. Latino Studies Faculty Scholarship. 19. https://scholarsarchive.library.albany.edu/lacs_fac_scholar/19 This Encyclopedia Entry is brought to you for free and open access by the Latin American, Caribbean, and U.S. Latino Studies at Scholars Archive. It has been accepted for inclusion in Latin American, Caribbean, and U.S. Latino Studies Faculty Scholarship by an authorized administrator of Scholars Archive. For more information, please contact [email protected]. 516 PUERTO RICO, COLONIALISM IN PUERTO RICO, COLONIALISM IN. Puerto Rico They automatically became subjects of the United States has been a colonial possession of the United States since without any constitutionally protected rights. Despite the 1898. What makes Puerto Rico a colony? The simple an humiliation of being denied any involvement in fateful swer is that its people lack sovereignty and are denied the decisions in Paris, most Puerto Ricans welcomed U.S. fundamental right to freely govern themselves. The U.S. sovereignty, believing that under the presumed enlight Congress exercises unrestricted and unilateral powers over ened tutelage of the United States their long history of Puerto Rico, although the residents of Puerto Rico do not colonial rule would soon come to an end. -
Cyperaceae of Puerto Rico. Arturo Gonzalez-Mas Louisiana State University and Agricultural & Mechanical College
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1964 Cyperaceae of Puerto Rico. Arturo Gonzalez-mas Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Gonzalez-mas, Arturo, "Cyperaceae of Puerto Rico." (1964). LSU Historical Dissertations and Theses. 912. https://digitalcommons.lsu.edu/gradschool_disstheses/912 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. This dissertation has been 64—8802 microfilmed exactly as received GONZALEZ—MAS, Arturo, 1923- CYPERACEAE OF PUERTO RICO. Louisiana State University, Ph.D., 1964 B o ta n y University Microfilms, Inc., Ann Arbor, Michigan CYPERACEAE OF PUERTO RICO A Dissertation I' Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Botany and Plant Pathology by Arturo Gonzalez-Mas B.S., University of Puerto Rico, 1945 M.S., North Carolina State College, 1952 January, 1964 PLEASE NOTE: Not original copy. Small and unreadable print on some maps. Filmed as received. UNIVERSITY MICROFILMS, INC. ACKNOWLEDGMENT The author wishes to express his sincere gratitude to Dr. Clair A. Brown for his interest, guidance, and encouragement during the course of this investigation and for his helpful criticism in the preparation of the manuscript and illustrations. -
Political Status of Puerto Rico: Brief Background and Recent Developments for Congress
Political Status of Puerto Rico: Brief Background and Recent Developments for Congress R. Sam Garrett Specialist in American National Government June 12, 2017 Congressional Research Service 7-5700 www.crs.gov R44721 Political Status of Puerto Rico: Brief Background and Recent Developments for Congress Summary Puerto Rico lies approximately 1,000 miles southeast of Miami and 1,500 miles from Washington, DC. Despite being far outside the continental United States, the island has played a significant role in American politics and policy since the United States acquired Puerto Rico from Spain in 1898. Puerto Rico’s political status—referring to the relationship between the federal government and a territorial one—is an undercurrent in virtually every policy matter on the island. In a June 11, 2017, plebiscite (popular vote), 97.2% of voters chose statehood when presented with three options on the ballot. Turnout for the plebiscite was 23.0% of eligible voters. Some parties and other groups opposing the plebiscite had urged their bases to boycott the vote. (These data are based on 99.5% of precincts reporting results.) After initially including only statehood and free association/independence options, an amended territorial law ultimately permitted three options on the plebiscite ballot: statehood, free association/independence, or current territorial status. Before the latest plebiscite, Puerto Ricans most recently reconsidered their status through a 2012 plebiscite. On that occasion, voters were asked two questions: whether to maintain the status quo, and if a change were selected, whether to pursue statehood, independence, or status as a “sovereign free associated state.” Majorities chose a change in the status quo in answering the first question, and statehood in answering the second. -
Bookletchart™ Bahía De Ponce and Approaches NOAA Chart 25683 a Reduced-Scale NOAA Nautical Chart for Small Boaters
BookletChart™ Bahía de Ponce and Approaches NOAA Chart 25683 A reduced-scale NOAA nautical chart for small boaters When possible, use the full-size NOAA chart for navigation. Published by the Channels.–The principal entrance is E of Isla de Cardona. A Federal project provides for a 600-foot-wide entrance channel 36 feet deep, National Oceanic and Atmospheric Administration then an inner channel 200-foot-wide 36 feet deep leading to an irregular National Ocean Service shaped turning basin, with a 950-foot turning diameter adjacent to the Office of Coast Survey municipal bulkhead. The entrance channel is marked by a 015° lighted range, lights, and www.NauticalCharts.NOAA.gov buoys; do not confuse the rear range light with the flashing red radio 888-990-NOAA tower lights back of it. A 0.2-mile-wide channel between Isla de Cardona and Las Hojitas is sometimes used by small vessels with local knowledge. What are Nautical Charts? Anchorages.–The usual anchorage is NE of Isla de Cardona in depths of 30 to 50 feet, although vessels can anchor in 30 to 40 feet NW of Las Nautical charts are a fundamental tool of marine navigation. They show Hojitas. A small-craft anchorage is NE of Las Hojitas in depths of 18 to 28 water depths, obstructions, buoys, other aids to navigation, and much feet. (See 110.1 and 110.255, chapter 2, for limits and regulations.) A more. The information is shown in a way that promotes safe and well-protected anchorage for small boats in depths of 19 to 30 feet is NE efficient navigation. -
Mesozoic and Cenozoic Sequence Stratigraphy of European Basins
Downloaded from http://pubs.geoscienceworld.org/books/book/chapter-pdf/3789969/9781565760936_frontmatter.pdf by guest on 26 September 2021 Downloaded from http://pubs.geoscienceworld.org/books/book/chapter-pdf/3789969/9781565760936_frontmatter.pdf by guest on 26 September 2021 MESOZOIC AND CENOZOIC SEQUENCE STRATIGRAPHY OF EUROPEAN BASINS PREFACE Concepts of seismic and sequence stratigraphy as outlined in To further stress the importance of well-calibrated chronos- publications since 1977 made a substantial impact on sedimen- tratigraphic frameworks for the stratigraphic positioning of geo- tary geology. The notion that changes in relative sea level shape logic events such as depositional sequence boundaries in a va- sediment in predictable packages across the planet was intui- riety of depositional settings in a large number of basins, the tively attractive to many sedimentologists and stratigraphers. project sponsored a biostratigraphic calibration effort directed The initial stratigraphic record of Mesozoic and Cenozoic dep- at all biostratigraphic disciplines willing to participate. The re- ositional sequences, laid down in response to changes in relative sults of this biostratigraphic calibration effort are summarized sea level, published in Science in 1987 was greeted with great, on eight charts included in this volume. albeit mixed, interest. The concept of sequence stratigraphy re- This volume also addresses the question of cyclicity as a ceived much acclaim whereas the chronostratigraphic record of function of the interaction between tectonics, eustasy, sediment Mesozoic and Cenozoic sequences suffered from a perceived supply and depositional setting. An attempt was made to estab- absence of biostratigraphic and outcrop documentation. The lish a hierarchy of higher order eustatic cycles superimposed Mesozoic and Cenozoic Sequence Stratigraphy of European on lower-order tectono-eustatic cycles. -
If^^-^^Ttsq ——Y National Register of Historic Places Multiple Property Documentation Form
NPS Form 10-900-b OMB No. 1024-0018 (June 1991) If^^-^^ttSQ ——y National Register of Historic Places Multiple Property Documentation Form This form is used for documenting multiple property groups relating to one or several historic contexts. See Multiple Property Documentation Form (National Register Bulletin 16B). Complete each item by entering the requested information. additional space, use continuation sheets (Form 10-900-a). Use a typewriter, word processor, or computer to complete all items. _X _ New Submission __ Amended Submission A. Name of Multiple Property Listing Ball Court / Plaza Sites of Puerto Rico and the U.S. Virgin Islands B. Associated Historic Contexts (Name each associated historic context, identifying theme, geographical area, and chronological period for each.) Ball Court / Plaza Sites of the prehistoric Early Ostionoid (pre-Taino) (AD 600-1200) and Late Ostionoid (Taino) (AD 1200-1500) periods village sites C. Form Prepared by name/title Mark R. Barnes. PhD - Senior Archaeoloist organization National Register Programs - NPS Southeast Region date July 9. 1999 street & number 1924 Bldg.-5th floor. 100 Alabama St. SW___ telephone (404)562-3173 city or town Atlanta ___________ state GA ____________ zip code 30303 ___________ D. Certification As the designated authority under the National Historic Preservation Act of 1966, as amended, I hereby certify that this documentation form meets the National Register documentation standards and sets forth requirements for the listing of related properties consistent with the National Register criteria. This submission meets the procedural and professional requirements set forth in 36 CFR Part 60 and the Secretary of the Interior's Standards and Guidelines for Archeology and Historic Preservation. -
Guide to Theecological Systemsof Puerto Rico
United States Department of Agriculture Guide to the Forest Service Ecological Systems International Institute of Tropical Forestry of Puerto Rico General Technical Report IITF-GTR-35 June 2009 Gary L. Miller and Ariel E. Lugo The Forest Service of the U.S. Department of Agriculture is dedicated to the principle of multiple use management of the Nation’s forest resources for sustained yields of wood, water, forage, wildlife, and recreation. Through forestry research, cooperation with the States and private forest owners, and management of the National Forests and national grasslands, it strives—as directed by Congress—to provide increasingly greater service to a growing Nation. The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable sex, marital status, familial status, parental status, religion, sexual orientation genetic information, political beliefs, reprisal, or because all or part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at (202) 720-2600 (voice and TDD).To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W. Washington, DC 20250-9410 or call (800) 795-3272 (voice) or (202) 720-6382 (TDD). USDA is an equal opportunity provider and employer. Authors Gary L. Miller is a professor, University of North Carolina, Environmental Studies, One University Heights, Asheville, NC 28804-3299.