HAMBRIGHT-BELUE Assistant Professor Aia Leed Ap

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SALLIE HAMBRIGHT-BELUE assistant professor aia leed ap 1884 1888 1898 1908 1920 composite 1920 tracing the shifting REEDY This competition entry proposes a wall that attempts to make visible the 1908 relationship between the city and the river. By tracing historical maps of AM11 Alteration Competition Entry AM11 the development of Greenville, SC, the Reedy River seems to have 1900 1898 shifted over time by the growing city. The shifting occurred over several years and over a large area which is imperceptible to those living in Greenville today. The installation would increase awareness of the tenu- 1888 1884 ous relationship between nature and cities. Falls St. Main St. Main St. Rhett St. Laurens St. River St. River St. Academy St. Cox St. The Pozzuoli waterfront site offers a unique and varied condition, which must influence any master plan. The unique qualities are in its land forma- tion, its topography, and in its history. These unique factors include: 1. Geological Centers of Activity and Fault Lines Pozzuoli is in the middle of a caldera which is an area of land that col- lapses after a volcanic eruption due to the release of magma from a magma chamber in the earth. The caldera surrounding Pozzuoli is called the Campi Flegrei, or the Phlegraean Fields. This caldera continues to be active because of magma remaining in the magma pocket and causes the land to move vertically and laterally. 2. Historically Modified Coastline The coastline has moved substantially since Roman times. During Roman times, the coastline was located about 230 meters further out in Pozzuoli Bay. In the 1700’s, the water moved substantially inland - entirely covering the current waterfront. 3. Historic Artifacts and Ruins The waterfront is anchored by two of the most interesting Roman ruins in Pozzuoli. In the east, Rione Terra, or the old city, is being excavated. In the west, Portus Julius, or the old port, lies just beneath the water’s sur- face. Other Roman ruins lie just along the waterfront like the Villa Livia, Pozzuoli, Italy Masterplan w/ Eisenman Architects Pozzuoli, Italy Masterplan w/ Eisenman the old stadium, and the Macellum..

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High Resolution Monitoring of Campi Flegrei (Naples, Italy) by Exploiting Terrasar-X Data: an Application to Solfatara Crater
HIGH RESOLUTION MONITORING OF CAMPI FLEGREI (NAPLES, ITALY) BY EXPLOITING TERRASAR-X DATA: AN APPLICATION TO SOLFATARA CRATER Christian Minet (1), Kanika Goel (1), Ida Aquino (2), Rosario Avino (2), Giovanna Berrino (2), Stefano Caliro (2), Giovanni Chiodini (2), Prospero De Martino (2), Carlo Del Gaudio (2), Ciro Ricco (2), Valeria Siniscalchi (2), Sven Borgstrom (2) (1)German Aerospace Center (DLR) IMF, Münchner Strasse 20, 82234 Wessling, Germany Email: [christian.minet, kanika.goel]@dlr.de (2)Istituto Nazionale di Geofisica e Vulcanologia, sezione di Napoli “Osservatorio Vesuviano” , via Diocleziano, 328, 80124 Naples, Italy Email: [email protected] ABSTRACT by continuous ground deformation (bradyseismic activity) related to its volcanic nature. Geodetic monitoring of Campi Flegrei caldera, west of In particular, we will focus on the Solfatara - Pisciarelli Naples (Italy), is carried out through integrated ground area, which is seat of strong fumarolic activity in the based networks and space-borne Differential InSAR last years. For this reason we also take into account (DInSAR) techniques, exploiting the SAR sensors some information from geochemical measurements. [3]. onboard ERS1-2 (till the end of their lifetime) and The geodetic monitoring of the area has been ENVISAT satellites. Unfortunately, C-band sensors historically carried out by the Osservatorio Vesuviano give no information when dealing with very low [4],[5],[6],[7], presently the Naples branch of the deformation rates and very small deforming areas. Istituto Nazionale di Geofisica e Vulcanologia To overcome these problems, we decided to use (INGV-OV) by ground based networks (levelling, TerraSAR-X from DLR, a high resolution SAR sensor EDM, gravity, tide-gauge, tiltmeter), shown in Fig.
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Campi Flegrei Caldera, Somma–Vesuvius Volcano, and Ischia Island) from 20 Years of Continuous GPS Observations (2000–2019)
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Plinian Pumice Fall Deposit of the Campanian Ignimbrite Eruption Ž/Phlegraean Fields, Italy
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M. Guidarelli1, A. Zille, A. Saraò1, M. Natale2, C. Nunziata2 and G.F. Panza1,3
Available at: http://www.ictp.it/~pub_off IC/2006/145 United Nations Educational, Scientific and Cultural Organization and International Atomic Energy Agency THE ABDUS SALAM INTERNATIONAL CENTRE FOR THEORETICAL PHYSICS SHEAR-WAVE VELOCITY MODELS AND SEISMIC SOURCES IN CAMPANIAN VOLCANIC AREAS: VESUVIUS AND PHLEGRAEAN FIELDS M. Guidarelli1, A. Zille, A. Saraò1, M. Natale2, C. Nunziata2 and G.F. Panza1,3 1 Dipartimento di Scienze della Terra, Università degli Studi di Trieste, Trieste, Italy 2 Dipartimento di Geofisica e Vulcanologia, Università di Napoli “Federico II”, Napoli, Italy 3 The Abdus Salam International Centre for Theoretical Physics, Trieste, Italy MIRAMARE – TRIESTE December 2006 Abstract This chapter summarizes a comparative study of shear-wave velocity models and seismic sources in the Campanian volcanic areas of Vesuvius and Phlegraean Fields. These velocity models were obtained through the nonlinear inversion of surface- wave tomography data, using as a priori constraints the relevant information available in the literature. Local group velocity data were obtained by means of the frequency-time analysis for the time period between 0.3 and 2 s and were combined with the group velocity data for the time period between 10 and 35 s from the regional events located in the Italian peninsula and bordering areas and two station phase velocity data corresponding to the time period between 25andl00s.In order to invert Ray lei gh wave dispersion curves, we applied the nonlinear inversion method called hedgehog and retrieved average models for the first 30-35 km of the lithosphere, with the lower part of the upper mantle being kept fixed on the basis of existing regional models.
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Campania/Rv Schoder. Sj
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