The life of Sir Anthony Panizzi, K.C.B., late principal librarian of the British Museum, senator of Italy /

Mode of access: Internet.

The life and correspondence of Sir Anthony Panizzi, k.c. b., late principal librarian of the British museum, senator of Italy, etc. In two volumes.

The proposed third volume was never published, although copyright claim is printed on back of t.-p. ("The Reminiscences copyright 1881 by Henry Stevens of Vermont." The records of the Copyright office do not bear out this statement) The material was later published in Transactions and proceedings of the Library association of the United Kingdom at their seventh annual meeting...1884. London, 1890 (p. 117-124: Twenty years reminiscences of Panizzi and the British museum, 1845-1865)

Report of Agricultural Commission to Europe. Observations made by American agriculturists in Great Britain, France, and Italy for the United States Department of Agriculture.

Mode of access: Internet.

The dawn of Italian independence: Italy from the Congress of Vienna, 1914, to the fall of Venice, 1849.

Mode of access: Internet.

Calendar of state papers and manuscripts: relating to English affairs existing in the archives and collection of Venice, and in other libraries of northern Italy.

Vol. 6:3 and v. 7: Nendeln, Liechtenstein: Kraus reprint, 1970.

The humanism of Italy : book I of Thought and expression in the sixteenth century /

Includes bibliographical references.

The life of Henry John Temple, viscount Palmerston: 1846-1865.

A continuation of Bulwer's Life of Palmerston.

The problem of the immigrant; a brief discussion, with a summary of conditions, laws, and regulations governing the movement of population to and from the British empire, United States, France, Belgium, Switzerland, Germany, Italy, Austria-Hungary, Spain, Portugal, Netherlands, Denmark, Scandinavia and Russia:

Mode of access: Internet.

Coryate's crudities; hastily gobled up in five months travels in France, Savoy, Italy, Rhetia commonly called the Grisons country, Helvetia alias Switzerland, some parts of high Germany and the Netherlands; newly digested in the hungry aire of Odcombe in the county of Somerset, and now dispersed to the nourishment of the travelling members of this kingdome,

Special t.p.: Posthuma fragmenta poematum Georgii Coryati Sarisburiensis, sacrae theologiae baccalaurei, quondem e sociis Novi collegii in inclyta academia Oxoniensi, as postea ecclesiae Odcombiensis in agro Somersetensi ministri, ubi tandem anno 1606, extremum vitae diem clausit. Londini, anno domini 1611: vol.II, p. [377-408]

The problem of the immigrant : a brief discussion, with a summary of conditions, laws, and regulations governing the movement of population to and from the British empire, United States, France, Belgium, Switzerland, Germany, Italy, Austria-Hungary, Spain, Portugal, Netherlands, Denmark, Scandinavia and Russia /

Includes index.

Palaeoclimatic implications of the growth history and stable isotope (delta O-18 and delta C-13) geochemistry of a Middle to Late Pleistocene stalagmite from central-western Italy

The age structure and, stable isotope composition of a stalagmite (CC I) from an upland cave in central-western Italy were studied to investigate regional response to global climatic changes. Four growth phases are constrained by 28 thermal ionization and multi-collector inductively coupled plasma mass spectrometry Th-U ages and reveal intermittent deposition through the period between Marine isotope Stage (MIS) 11 and 3 (similar to380 and similar to43 kyr). Most of the growth took place between similar to380 and similar to280 kyr, a period punctuated briefly by a hiatus in deposition through the glacial maximum of MIS 10. Growth was terminated abruptly at 280 kyr just prior to the MIS 8 glacial maximum. With a present-day chamber temperature of 7.5 degreesC, the timing of hiatuses close to these glacial maxima point to freezing conditions at the time. No deposition was recorded through the entirety of MIS 7 and most of MIS 6, whilst two minor growth phases occurred at similar to141-125 and similar to43 kyr. Growth at 141 kyr indicates temperatures >0 degreesC at a time when MIS 6 ice volumes were close to their maximum. High stable carbon isotope (delta(13)C) values (similar to2.8parts per thousand to +3.1parts per thousand) throughout the stalagmite's growth reflect a persistently low input of biogenic CO2, indicating that the steep, barren and alpine-like recharge area of today ha's been in existence for at least the last similar to380 kyr. During MIS 9, the lowest delta(13)C values occur well after maximum interglacial conditions, suggesting a lag in the development of post-glacial soils in this high-altitude karst. The stable oxygen isotope (delta(18)O) trends match the main structural features of the major climate proxy records (SPECMAP, Vostok and Devils Hole), suggesting that the delta(18)O of CC1 has responded to global-scale climate changes, whilst remarkable similarity exists between CC1 delta(18)O and regional sea-surface temperature reconstructions from North Atlantic core ODP980 and southwest Pacific marine core MD97-2120 through the most detailed part of the CC1 record, MIS 9-8. The results suggest that CC1 and other stalagmites from the cave have the potential to capture a long record of regional temperature trends, particularly in regards to the relative severity of Pleistocene glacial stages. (C) 2004 Elsevier B.V. All rights reserved.

The tectonically-confined Firenzuola turbidite system (Miocene, Marnoso-arenacea Formation, northern Apennines, Italy): an example of facies variations related to the basin morphology

The Firenzuola turbidite system formed during a paroxysmal phase of thrust propagation, involving the upper Serravallian deposits of the Marnoso-arenacea Formation (MAF). During this phase the coeval growth of two major tectonic structures, the M. Castellaccio thrust and the Verghereto high, played a key role, causing a closure of the inner basin and a coeval shift of the depocentre to the outer basin. This work focuses on this phase of fragmentation of the MAF basin; it is based on a new detailed high-resolution stratigraphic framework, which was used to determine the timing of growth of the involved structures and their direct influence on sediment dispersal and on the lateral and vertical turbidite facies distribution. The Firenzuola turbidite system stratigraphy is characterized by the occurrence of mass-transport complexes (MTCs) and thick sandstone accumulation in the depocentral area, which passes to finer drape over the structural highs; the differentiation between these two zones increases over time and ends with the deposition of marly units over the structural highs and the emplacement of the Visignano MTC. According to the stratigraphic pattern and turbidite facies characteristics, the Firenzuola System has been split into two phases, namely Firenzuola I and Firenzuola II: the former is quite similar to the underlying deposits, while the latter shows the main fragmentation phase, testifying the progressive isolation of the inner basin and a coeval shift of the depocentre to the outer basin. The final stratigraphic and sedimentological dataset has been used to create a quantitative high-resolution 3D facies distribution using the Petrel software platform. This model allows a detailed analysis of lateral and vertical facies variations that can be exported to several reservoirs settings in hydrocarbon exploration and exploitation areas, since facies distributions and geometries of the reservoir bodies of many sub-surface turbidite basins show a significant relationship to the syndepositional structural activity, but are beyond seismic resolution.