Sinkhole Genesis and Evolution in Apulia, and Their Interrelations with the Anthropogenic Environment M
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Fenomeni Di Subsidenza Carsica
PROBLEMATICHE CONNESSE A FENOMENI DI SUBSIDENZA CARSICA E SINKHOLES IN PUGLIA DELLE ROSE MARCO*, FEDERICO ANTONIO** & PARISE MARIO* *CNR-IRPI, sezione di Bari **II Facoltà di Ingegneria (Taranto) - Politecnico di Bari INTRODUZIONE La regione Puglia presenta distinti contesti geologici con differenti condizioni di propen- sione al dissesto idrogeologico e di vulnerabilità ambientale. Tra queste, data la natura prevalentemente carbonatica delle rocce affioranti, i fenomeni di subsidenza carsica e di sprofondamento (sinkholes) hanno un ruolo notevole. Negli ultimi decenni sono stati, infatti, registrati numerosi eventi, alcuni dei quali hanno arrecato danni a strutture antropiche presenti sul territorio. Il presente contributo intende esaminare, dopo una introduzione agli aspetti generali del carsismo del territorio pugliese, le principali pro- blematiche relative a questo tipo di fenomeni sulla base di alcuni casi di studio. 1. ASSETTO GEOLOGICO E FENOMENI DI SINKHOLES I territori carsici sono caratterizzati da peculiari aspetti geologici, morfologici e idrogeo- logici, che li rendono particolarmente inclini allo sviluppo di fenomeni di subsidenza e di sinkholes (NICOD, 1972; WHITE, 1988). La solubilità delle rocce carbonatiche, e il conse- guente sviluppo ed evoluzione di processi carsici e speleogenetici (FORD, 1988) si combi- nano in tali ambienti all’azione antropica, di frequente producendo situazioni di rischio. Fig. 1 - Schema geologico della Puglia, con indicazione dei casi citati nel testo. Legenda: 1) depo- siti alluvionali, argille e calcareniti (Pliocene – Pleistocene); 2) rocce carbonatiche bioclastiche (Paleogene) e calcareniti (Miocene); 3) rocce di piattaforma carbonatica (Cretaceo). 377 La Regione Puglia è prevalentemente caratterizzata dall’affioramento di rocce carbona- tiche, per cui i processi carsici risultano di estrema rilevanza praticamente sull’intero territorio. -
Introduction to Virginia's Karst
Introduction to Virginia’s Karst A presentation of The Virginia Department of Conservation and Recreation’s Karst Program & Project Underground Karst - A landscape developed in limestone, dolomite, marble, or other soluble rocks and characterized by subsurface drainage systems, sinking or losing streams, sinkholes, springs, and caves. Cross-section diagram by David Culver, American University. Karst topography covers much of the Valley and Ridge Province in the western third of the state. Aerial photo of karst landscape in Russell County. Smaller karst areas also occur in the Cumberland Plateau, Piedmont, and Coastal Plain provinces. At least 29 counties support karst terrane in western Virginia. In western Virginia, karst occurs along slopes and in valleys between mountain ridges. There are few surface streams in these limestone valleys as runoff from mountain slopes disappears into the subsurface upon contact with the karst bedrock. Water flows underground, emerging at springs on the valley floor. Thin soils over fractured, cavernous limestone allow precipitation to enter the subsurface directly and rapidly, with a minimal amount of natural filtration. The purer the limestone, the less soil develops on the bedrock, leaving bare pinnacles exposed at the ground surface. Rock pinnacles may also occur where land use practices result in massive soil loss. Precipitation mixing with carbon dioxide becomes acidic as it passes through soil. Through geologic time slightly acidic water dissolves and enlarges the bedrock fractures, forming caves and other voids in the bedrock. Water follows the path of least resistance, so it moves through voids in rock layers, fractures, and boundaries between soluble and insoluble bedrock. -
Paesaggi Di Pietra
Geologia dell’Ambiente Supplemento al n. 3/2020 Periodico trimestrale della SIGEA ISSN 1591-5352 Società Italiana di Geologia Ambientale ATTI DEI CONVEGNI SUI PAESAGGI DI PIETRA PERETO (AQ) 9 AGOSTO 2019 A CURA DI GIUSEPPE GISOTTI OSTUNI (BR) 18 OTTOBRE 2019 A CURA DI EMANUELE GIACCARI EVENTI IN SICILIA Poste Italiane S.p.a. - Spedizione in Abbonamento Postale - D.L. 353/2003 (conv. in L. 27/02/2004 n° 46) art. 1 comma 1 - DCB Roma n° 46) art. 1 comma in L. 27/02/2004 (conv. 353/2003 - D.L. Postale - Spedizione in Abbonamento Italiane S.p.a. Poste 2019 A CURA DI MICHELE ORIFICI Società Italiana di Geologia Ambientale Associazione di protezione ambientale a carattere nazionale riconosciuta dal Ministero dell’ambiente, Sommario della tutela del territorio e del mare con D.M. 24/5/2007 e con successivo D.M. 11/10/2017 PRESIDENTE Antonello Fiore CONSIGLIO DIRETTIVO NAZIONALE Lorenzo Cadrobbi, Franco D’Anastasio (Segretario), Daria Duranti (Tesoriere), Ilaria Falconi, Antonello Fiore (Presidente), Sara Frumento, Presentazione Fabio Garbin, Enrico Gennari, Giuseppe Gisotti Giuseppe Gisotti, Emanuele Giaccari, Michele Orifici 3 (Presidente onorario), Gioacchino Lena, Luciano Masciocco, Michele Orifici (Vicepresidente), Vincent Ottaviani (Vicepresidente), Paola Pino d’Astore, Livia Soliani PERETO Geologia dell’Ambiente A cura di Giuseppe Gisotti Periodico trimestrale della SIGEA La calce a Pereto (L’Aquila) Supplemento al N. 3/2020 Anno XXVIII • luglio-settembre 2020 Massimo Basilici 9 Iscritto al Registro Nazionale della Stampa n. 06352 Autorizzazione -
Sinkhole Physical Models to Simulate and Investigate Sinkhole Collapses
SINKHOLE PHYSICAL MODELS TO SIMULATE AND INVESTIGATE SINKHOLE COLLAPSES Mohamed Alrowaimi Doctoral Student, Civil, Environmental and Construction Engineering, University of Central Florida, 4000 Central Florida Blvd., Orlando, Florida, 32816, USA, [email protected] Hae-Bum Yun Assistant professor, Civil, Environmental and Construction Engineering, University of Central Florida, 4000 Central Florida Blvd., Orlando, Florida, 32816, USA, [email protected] Manoj Chopra Professor, Civil, Environmental and Construction Engineering, University of Central Florida 4000 Central Florida Blvd., Orlando, Florida, 32816, USA, [email protected] Abstract Introduction Florida is one of the most susceptible states for sinkhole Sinkhole is a ground surface depression that occurs with collapses due to its karst geology. In Florida, sinkholes or without any surface indication. Sinkholes commonly are mainly classified as cover subsidence sinkholes that occur in a very distinctive terrain called karst terrain. result in a gradual collapse with possible surface signs, This terrain mainly has a bedrock of a carbonate rocks and cover collapse sinkholes, which collapse in a sudden such as limestone, dolomite, or gypsum. Sinkholes and often catastrophic manner. The future development develop when the carbonate bedrocks are subjected of a reliable sinkhole prediction system will have to dissolution with time to form cracks, conduits, and the potential to minimize the risk to life, and reduce cavities in the underground bedrock. These features delays in construction due to the need for post-collapse allow the overburden soils (on top of the carbonate remediation. In this study, different versions of small- bedrock) to transport through them to the underground scale sinkhole physical models experimentally used cavities, which results in surface collapse due to the to monitor the water levels in a network of wells. -
Apulia a Journey Across All Seasons
Apulia A Journey across All Seasons Pocket Guide Mario Adda Editore Regione Puglia AreA Politiche Per lA Promozione del territorio, dei sAPeri e dei tAlenti Servizio Turismo – Corso Sonnino, 177 – cap 70121 Bari Tel. +39 080.5404765 – Fax +39 080.5404721 e-mail: [email protected] www.viaggiareinpuglia.it Text: Stefania Mola Translation: Christina Jenkner Photographs: Nicola Amato and Sergio Leonardi Drawings: Saverio Romito Layout: Vincenzo Valerio ISBN 9788880829362 © Copyright 2011 Mario Adda Editore via Tanzi, 59 - Bari Tel. e fax +39 080 5539502 www.addaeditore.it [email protected] Contents A Journey across All Seasons ....................................................pag. 7 A History ............................................................................................ 9 Buried Treasures ....................................................................................... 11 Taranto’s Treasure ........................................................................ 12 Egnazia ....................................................................................... 12 The Bronzes of Brindisi ............................................................... 13 The Vases of Ruvo ....................................................................... 13 Between Legend and Reality on the Hill of Cannae ....................... 14 Ostuni – Pre-Classical Civilizations ............................................... 14 Caves and Prayers ....................................................................... -
The Favorability of Florida's Geology to Sinkhole
Appendix H: Sinkhole Report 2018 State Hazard Mitigation Plan _______________________________________________________________________________________ APPENDIX H: Sinkhole Report _______________________________________________________________________________________ Florida Division of Emergency Management THE FAVORABILITY OF FLORIDA’S GEOLOGY TO SINKHOLE FORMATION Prepared For: The Florida Division of Emergency Management, Mitigation Section Florida Department of Environmental Protection, Florida Geological Survey 3000 Commonwealth Boulevard, Suite 1, Tallahassee, Florida 32303 June 2017 Table of Contents EXECUTIVE SUMMARY ............................................................................................................ 4 INTRODUCTION .......................................................................................................................... 4 Background ................................................................................................................................. 5 Subsidence Incident Report Database ..................................................................................... 6 Purpose and Scope ...................................................................................................................... 7 Sinkhole Development ................................................................................................................ 7 Subsidence Sinkhole Formation .............................................................................................. 8 Collapse Sinkhole -
Caves in New Mexico and the Southwest Issue 34
Lite fall 2013 Caves in New Mexico and the Southwest issue 34 The Doll’s Theater—Big Room route, Carlsbad Cavern. Photo by Peter Jones, courtesy of Carlsbad Caverns National Park. In This Issue... Caves in New Mexico and the Southwest Cave Dwellers • Mapping Caves Earth Briefs: Suddenly Sinkholes • Crossword Puzzle New Mexico’s Most Wanted Minerals—Hydromagnesite New Mexico’s Enchanting Geology Classroom Activity: Sinkhole in a Cup Through the Hand Lens • Short Items of Interest NEW MEXICO BUREAU OF GEOLOGY & MINERAL RESOURCES A DIVISION OF NEW MEXICO TECH http://geoinfo.nmt.edu/publications/periodicals/litegeology/current.html CAVES IN NEW MEXICO AND THE SOUTHWEST Lewis Land Cave Development flowing downward from the surface. Epigenic A cave is a naturally-formed underground cavity, usually caves can be very long. with a connection to the surface that humans can enter. The longest cave in the Caves, like sinkholes, are karst features. Karst is a type of world is the Mammoth landform that results when circulating groundwater causes Cave system in western voids to form due to dissolution of soluble bedrock. Karst Kentucky, with a surveyed terrain is characterized by sinkholes, caves, disappearing length of more than 400 streams, large springs, and underground drainage. miles (643 km). The largest and most common caves form by dissolution of In recent years, limestone or dolomite, and are referred to as solution caves. scientists have begun to Limestone and dolomite rock are composed of the minerals recognize that many caves calcite (CaCO ) and dolomite (CaMg(CO ) ), which are 3 3 2 are hypogenic in origin, soluble in weak acids such as carbonic acid (H CO ), and are 2 3 meaning that they were thus vulnerable to dissolution by groundwater. -
Cave Diving in Southeastern Pennsylvania
The Underground Movement Volume 13, Number 11 CAVE DIVING IN SOUTHEASTERN PENNSYLVANIA November 2013 CAVE DIVING IN SOUTHEASTERN PENNSYLVANIA An Historical, Cultural, and Speleological Perspective of Bucks County — Danny A. Brass — Large portions of central and southern Pennsylvania are ipants than dry caving, cave diving still remains a global underlain by carbonate bedrock (primarily limestone and activity. Worldwide, a variety of cave-diving organiza- dolomite, but with smaller amounts of marble as well). tions can be found in areas rich in underwater caves. Ma- Over the course of geologic time, much of this bedrock jor cave-diving sites include the cenotes and tidal blue- has been exposed by gradual erosion of the overburden. holes of the Bahamas and Mexico’s Yucatán Peninsula, In combination with the abrasive activity of water-borne the vast underground rivers of Australia’s Nullarbor Plain sediments, the relentless action of weak acids (i.e., chemi- and the sinkholes of its unique Mt. Gambier region, the cal dissolution by acidic groundwater) on soluble car- sumps of Great Britain, and the rich concentration of bonate deposits, especially limestone, is a self- springs in Florida. Diving conditions vary greatly from accelerating process that has led to the development of one region to another. This is reflected in the many differ- broad areas of karst topography. A variety of surface and ences in training procedures, required equipment, under- subsurface geological features are characteristically asso- water protocols, and even diving philosophies, all of ciated with karstification; the presence of large numbers which have evolved in association with local diving con- of solution caves and sinkholes is common. -
Understanding Zacaton: Exploration and Initial
Karst Frontiers Gary 141 Karst WatersInstitute SpecialPublication 7 UNDERSTANDING ZACATON: EXPLORATION AND INITIAL INTERPRET A TION OF THE WORLDS DEEPEST KNOWN PHREATIC SINKHOLE AND RELATED KARST FEA TURES SOUTHERN T AMA ULIP AS, MEXICO Marcus Gary The University of Texasat Austin/ United StatesGeological Survey 8027 ExchangeDrive Austin, TX 78754 [email protected] A system of water-filled sinkholes (known as cenotes) this extreme karst system have taken place, and it has only exists in southern Tamaulipas, Mexico (Figure 1), and is been limited work within the past two years that theories the result of a unique combination of speleogenetic factors. relating to the speleogenesishave been formed. Microbial This system is composed of 18 different karst features that interaction seems likely to affect karstification processes, are on or near a large cattle ranch known as Rancho La and significant travertine structures appear to have a direct Azufrosa. Zacat6n, the deepest cenote in this system has influence on the hydraulic connectivity between the bodies been measured to over 350 meters deep, (Figure 1) and is of water. Years of future research are being planned to the site of the world-record SCUBA dive (284 meters) by document the extent of karstification in this deep Jim Bowden in 1994 (Gilliam, 1994). This makes it the hydrothermal system and interpret the geological history deepest known water-filled pit that has been explored by that has develope~ such an impressive example of humans in the world. No previous scientific studies of hypogenetic karst. Figure 1: Generalized cross section of the cenotes of Rancho La Azufrosa. -
Final Report
Biological Inventory of the Cave and Karst Systems of The Nature Conservancy’s Sharp-Bingham Mountain Preserve James Godwin Alabama Natural Heritage Program Environmental Institute Auburn University Auburn, AL 36849 ©Alan Cressler 1 Introduction Overview of Karst and Caves (adapted from Palmer 2007; White 2008) Karst is a landform or landscape with the characteristics of caves, sinkholes, subterranean streams, and springs. These topographical features have formed from the dissolution, rather than mechanical, eroding of the underlying bedrock. This dissolutional process is based on the actions of a weak carbonic acid solution reacting with the basic limestone. Raindrops, as they pass through the atmosphere, pick up carbon dioxide and form a weak carbonic acid solution. Limestone, a type of calcium carbonate, is easily dissolved by this mildly acidic water. Over time rainwater percolates along horizontal and vertical fissures and joints of the limestone bedrock and these joints and fissures gradually become widened and deepened, eventually coalescing into an underground drainage system of conduits. Caves formed by this process are termed solution caves. While the lifespan of a cave, from the initial phase of development to deterioration, may be on the order of tens of thousands to a few million years, geologically they are regarded as being transient. Cave “life history” can be divided into the following sequential phases: initiation, enlargement, stagnation, and destruction. Each phase in the life cycle of a cave presents new invasion and niche expansion opportunities for organisms associated with these subterranean features. During the phase of initiation, as water moves through a multitude of fissures dissolving bedrock, the smallest fissures of 10 to 50 micrometers wide are enlarged to widths of 5 to 10 millimeters. -
Journal of Cave and Karst Studies
March 2018 Volume 80, Number 1 JOURNAL OF ISSN 1090-6924 A Publication of the National CAVE AND KARST Speleological Society STUDIES DEDICATED TO THE ADVANCEMENT OF SCIENCE, EDUCATION, EXPLORATION, AND CONSERVATION Published By BOARD OF EDITORS The National Speleological Society Anthropology George Crothers http://caves.org/pub/journal University of Kentucky Lexington, KY Office [email protected] 6001 Pulaski Pike NW Huntsville, AL 35810 USA Conservation-Life Sciences Tel:256-852-1300 Julian J. Lewis & Salisa L. Lewis Lewis & Associates, LLC. [email protected] Borden, IN [email protected] Editor-in-Chief Earth Sciences Benjamin Schwartz Malcolm S. Field Texas State University National Center of Environmental San Marcos, TX Assessment (8623P) [email protected] Office of Research and Development U.S. Environmental Protection Agency Leslie A. North 1200 Pennsylvania Avenue NW Western Kentucky University Washington, DC 20460-0001 Bowling Green, KY [email protected] 703-347-8601 Voice 703-347-8692 Fax [email protected] Mario Parise University Aldo Moro Production Editor Bari, Italy Scott A. Engel [email protected] Knoxville, TN 225-281-3914 Exploration Paul Burger [email protected] National Park Service Eagle River, Alaska Journal Copy Editor [email protected] Linda Starr Microbiology Albuquerque, NM Kathleen H. Lavoie State University of New York Plattsburgh, NY [email protected] Paleontology Greg McDonald National Park Service Fort Collins, CO [email protected] Social Sciences Joseph C. Douglas The Journal of Cave and Karst Studies , ISSN 1090-6924, CPM Volunteer State Community College Number #40065056, is a multi-disciplinary, refereed journal pub- Gallatin, TN lished four times a year by the National Speleological Society. -
GEOLOGICAL and GEOMORPHOLOGICAL CONTROLS on FLOOD PHENOMENA in the PUTIGNANO TOWN, SOUTHERN ITALY Paolo Giannandrea 1, Salvatore
Available online http://amq.aiqua.it ISSN (print): 2279-7327, ISSN (online): 2279-7335 Alpine and Mediterranean Quaternary, 31 (2), 2018, 221 - 234 https://doi.org/10.26382/AMQ.2018.17 GEOLOGICAL AND GEOMORPHOLOGICAL CONTROLS ON FLOOD PHENOMENA IN THE PUTIGNANO TOWN, SOUTHERN ITALY Paolo Giannandrea 1, Salvatore Laurita 1, Francesca Pugliese 2 1 Dipartimento di Scienze, Università degli Studi della Basilicata, Potenza, Italy 2 Via Roma, 13, 70017 Putignano (BA), Italy Corresponding author: P. Giannandrea <[email protected]> ABSTRACT: The geological/geomorphological map of Putignano town (Bari, Southern Italy) contains useful evidence of landforms and sedimentary successions in both urbanized and industrial areas, contributing also to a better understanding of floodings dur- ing high-magnitude pluviometric events in the area. The analyzed flooded areas correspond to surfaces karst landforms with differ- ent shapes and sizes. Our detailed geological/geomorphological study shows that most of the industrial area of Putignano was built on Cretaceous calcareous units in a depressed area, which corresponds to an extensive endorheic basin (locally called "il Basso"). Part of the local urban expansion, built from 1950 to present day, occupies the most depressed areas of numerous karst valleys that, despite this urbanization, still preserve their hydraulic function. Usually these geological and geomorphological fea- tures are not yet completely identified and, unfortunately, not taken into consideration in the planning stages of the urban expan- sion and industrial settlement. Keywords: Putignano town, southern Italy, Apulian Foreland, Quaternary, flood, karst 1. INTRODUCTION thropogenic deposits. Putignano is a small town in the south-eastern 2. GEOLOGICAL AND GEOMORPHOLOGICAL Murge, an area frequently exposed to alluvial events SETTING OF THE MURGE RELIEF that occur despite the numerous mitigation actions tak- en to reduce or eliminate long-term risk to people and The carbonate rocks of the Murge hills, with the infrastructure.