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Libri sul tema "Cyclist Corps"

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Autore: Grafiati
Pubblicato: 25 luglio 2024
Ultima modifica: 31 luglio 2024

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1

Austin, Ronald J. Cycling to war: The history of the AIF/NZ Cyclist Corps 1916-1919. McCrae, Vic: Slouch Hat Publications, 2008.

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2

NEW ZEALAND CYCLIST CORPS IN THE GREAT WAR 1914-1918. Naval & Military Press, 2006.

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3

New Zealand Cyclist Corps in the Great War 1914-1918 (Officers of the Regiment). Naval & Military Press, 2004.

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4

Correa, Mariana. ENTRAINEMENT COMPLET AU POIDS Du CORPS POUR CYCLISTES: LES MEILLEURS EXERCICES Et ENTRAINEMENTS CALLISTHENIQUES POUR DEVENIR UN FANTASTIQUE CYCLISTE. Createspace Independent Publishing Platform, 2016.

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5

Correa, Mariana. ENTRAINEMENT COMPLET AU POIDS Du CORPS POUR CYCLISTES SECONDE EDITION: LES MEILLEURS EXERCICES ET ENTRAINEMENTS CALLISTHENIQUES POUR DEVENIR Un FANTASTIQUE CYCLISTE. Createspace Independent Publishing Platform, 2018.

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6

Correa, Mariana. DU CYCLISTE MOYEN Au CYCLISTE PRODIGIEUX DEUXIEME EDITION: PREPAREZ VOTRE CORPS Et VOTRE ESPRIT POUR LA MEILLEURE SORTIE DE VOTRE VIE. Createspace Independent Publishing Platform, 2018.

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7

The great bicycle experiment: The Army's historic Black Bicycle Corps, 1896-97. Missoula, Mont: Mountain Press Pub. Co., 2012.

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8

Ellam, Rob. 7. Reconstructing the past and weathering the future. Oxford University Press, 2016. http://dx.doi.org/10.1093/actrade/9780198723622.003.0007.

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Abstract (sommario):
Tiny microfossils called Foraminifera form calcium carbonate shells that record the δ18O composition of the seawater in which they grew. These microfossils are found in sea bed sediment cores, and a lot of information from these oxygen isotope records can be extracted. ‘Reconstructing the past and weathering the future’ looks at the methodology used in palaeoclimate studies and explains gain and phase modelling and Milankovitch orbital cycles. Similar isotope temperature records have been constructed from polar ice cores. Atmospheric CO2 composition can be reconstructed from the amount of CO2 dissolved in the ice. A new sub-discipline of clumped isotope geochemistry—‘isotomics’—will have applications far beyond carbonate palaeothermometry.
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9

Sammons, Benjamin. Device and Composition in the Greek Epic Cycle. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780190614843.001.0001.

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Abstract (sommario):
From a corpus of Greek epics known in antiquity as the “Epic Cycle,” six poems dealt with the same Trojan War mythology as the Homeric poems. Though they are now lost, these poems were much read and much discussed in ancient times, not only for their content but for their mysterious relationship with the more famous works attributed to Homer. This study shows that these lost poems belonged, compositionally, to essentially the same tradition as the Homeric poems. It demonstrates that various compositional devices well-known from the Homeric epics were also fundamental to the narrative construction of these later works. Yet while the “cyclic” poets constructed their works using the same traditional devices as Homer, they used these to different ends and with different results. The essential difference between cyclic and Homeric epics lies not in the fundamental building blocks from which they are constructed, but in the scale of these components relative to the overall construction of poems. This sheds important light on the early history of epic as a genre, since it is likely that these devices originally developed to provide large-scale structure to shorter poems and have been put to quite different use in the composition of the monumental Homeric epics. This study includes many new suggestions about the overall form of lost cyclic epics and about the meaning and context of the few surviving verse fragments.
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10

Lurcock, Pontus, e Fabio Florindo. Antarctic Climate History and Global Climate Changes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190676889.013.18.

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Abstract (sommario):
Antarctic climate changes have been reconstructed from ice and sediment cores and numerical models (which also predict future changes). Major ice sheets first appeared 34 million years ago (Ma) and fluctuated throughout the Oligocene, with an overall cooling trend. Ice volume more than doubled at the Oligocene-Miocene boundary. Fluctuating Miocene temperatures peaked at 17–14 Ma, followed by dramatic cooling. Cooling continued through the Pliocene and Pleistocene, with another major glacial expansion at 3–2 Ma. Several interacting drivers control Antarctic climate. On timescales of 10,000–100,000 years, insolation varies with orbital cycles, causing periodic climate variations. Opening of Southern Ocean gateways produced a circumpolar current that thermally isolated Antarctica. Declining atmospheric CO2 triggered Cenozoic glaciation. Antarctic glaciations affect global climate by lowering sea level, intensifying atmospheric circulation, and increasing planetary albedo. Ice sheets interact with ocean water, forming water masses that play a key role in global ocean circulation.
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11

Lurcock, Pontus, e Fabio Florindo. Antarctic Climate History and Global Climate Changes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190699420.013.18.

Testo completo
Abstract (sommario):
Antarctic climate changes have been reconstructed from ice and sediment cores and numerical models (which also predict future changes). Major ice sheets first appeared 34 million years ago (Ma) and fluctuated throughout the Oligocene, with an overall cooling trend. Ice volume more than doubled at the Oligocene-Miocene boundary. Fluctuating Miocene temperatures peaked at 17–14 Ma, followed by dramatic cooling. Cooling continued through the Pliocene and Pleistocene, with another major glacial expansion at 3–2 Ma. Several interacting drivers control Antarctic climate. On timescales of 10,000–100,000 years, insolation varies with orbital cycles, causing periodic climate variations. Opening of Southern Ocean gateways produced a circumpolar current that thermally isolated Antarctica. Declining atmospheric CO2 triggered Cenozoic glaciation. Antarctic glaciations affect global climate by lowering sea level, intensifying atmospheric circulation, and increasing planetary albedo. Ice sheets interact with ocean water, forming water masses that play a key role in global ocean circulation.
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12

Stiglitz, Joseph E. The Roaring Nineties: A New History of the World's Most Prosperous Decade. W. W. Norton & Company, 2004.

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13

Stiglitz, Joseph E. The Roaring Nineties. Allen Lane, 2003.

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14

Stiglitz, Joseph E. The Roaring Nineties: A New History of the World's Most Prosperous Decade. W. W. Norton & Company, 2004.

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15

Stiglitz, Joseph E. The Roaring Nineties: A New History of the World's Most Prosperous Decade (Open Market Edition). W. W. Norton & Company, 2003.

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