La Imagen del Viaje a a Efeso en el Yambo XIII de Calícamo

El Yambo XIII de Calímaco (fr. 203 Pf.) es conocido, junto con el Yambo I, por su naturaleza programática y por su tono polémico: el poeta disputa con sus detractores, quienes lo acusan por la "variedad formal" (polieídeia) de sus obras. Entre las críticas que recibe, se cuenta la de "no haber viajado a Efeso", patria de Hiponacte, yambógrafo de fines del VI siglo a. C., a quien se atribuye la invención del metro coliámbico que Calímaco adopta en la composición de su poema. Esa imagen, la de una travesía no emprendida, habrá de ser vinculada con el mencionado concepto de polieídeia y con los alcances que la metáfora del viaje adquiere, tanto en la tradición de los poetas precedentes como en otras obras del propio alejandrino

Sediments and tephra layers from the southern Tyrrhenian abyssal plain near Marsili Seamount

From the south-eastern Tyrrhenian deep-sea floor, four sediment cores of "Meteor" cruise 22 (1971) are described. These cores were taken in the basin between the Aeolian Islands and the Marsili Seamount, an elevation of more tha 3000 m above the sea floor. The sedimentation of the deep-sea basin is distinguished by a sequence of turbidites with a high sedimentation rate. The composition of the clastic material and the position of the cores in the mouth area of the morphologically very pronounced Stromboli Canyon suggest an interpretation of the turbidite sequence as fan of this canyon onto the deep-sea floor. A white rhyolitic pumice-tephra at the base of the 4 m thick sequence of turbidites in core M22-102 has been correlated with the Pelato eruption of the island of Liparo in the 6th century A.D. At the foot of the Marsili Seamount - apparently in morphologically elevated positions - the influence of the turbidite sedimentation increases, the rate of sedimentation is lower and stratigraphic omissions are probable. Here, rather compacted globigerina marls have been found in only 15 -25 cm depth. In addition, volcanic material in the form of lapilli layers, palagonitized ashes and detrital volcanic sands of the Marsili Seamount have been encountered in this area. An up to 3 cm thick layer of completely palagonitized basaltic ash intercalates with the marls at the base of two cores. Layers of very fresh olivine basaltic lapilli in core 103 and palagonitized lapilli of latitic composition in core 104 testify to an explosive submarine volcanism of the Marsili Seamount. According to the stratigraphy of core 103, the latest manifestations of this basaltic volcanism belong to the late Pleistocene (Emiliana huxleyi-zone of Nannoplankton stratigraphy) The basaltic lapilli are glassy to perhyaline with phenocrysts or microphenocrysts predominantely of olivine. The petrological character of the basaltic volcanites with high MgO, Ni, Cr and high MgO/FeO- and Ni/Co-ratios exhibits primitive basaltic features. These basalts clearly differ from basalts of the ocean floors, mid-ocean ridges and marginal basins. Prominent features are a missing iron-enrichment trend and low TiO2. Al2O3 tends to be high, as well as K2O and related trace elements (Ba, Sr). In spite of silica undrsaturation and high color index, the Marsili basalt exhibit some analogies with the calcalkaline basalts of the Aeolian arc, as well as the undersaturated basalts of some other circumoceanic areas.

La Imagen del Viaje a a Efeso en el Yambo XIII de Calícamo

El Yambo XIII de Calímaco (fr. 203 Pf.) es conocido, junto con el Yambo I, por su naturaleza programática y por su tono polémico: el poeta disputa con sus detractores, quienes lo acusan por la "variedad formal" (polieídeia) de sus obras. Entre las críticas que recibe, se cuenta la de "no haber viajado a Efeso", patria de Hiponacte, yambógrafo de fines del VI siglo a. C., a quien se atribuye la invención del metro coliámbico que Calímaco adopta en la composición de su poema. Esa imagen, la de una travesía no emprendida, habrá de ser vinculada con el mencionado concepto de polieídeia y con los alcances que la metáfora del viaje adquiere, tanto en la tradición de los poetas precedentes como en otras obras del propio alejandrino

Pollen profile from sediment core Höllerer See

(expanded by Eberhard Grüger, Göttingen) The site "Höllerer See" is a lake in the northern foreland of the Alps, about 30 km north of the city of Salzburg/Austria, situated in the south-western part of Oberösterreich/Austria. A 2 m long piston core from this locality, consisting entirely of calcareous gyttja, was studied by pollen analysis. The three lowermost samples (1.98, 1.95 and 1.92 m) were deposited during the Preboreal when Pinus and Betula were still the dominating forest trees. High pollen values of thermophilous woody species (mainly Corylus and Quercus, but also Ulmus, Tilia, Fraxinus) prove the Boreal age of the next younger sample (1.91 m). The following two pollen spectra attest that Alnus (1.89 m) and - later (1.88 m) - Fagus had become important members of the local (Alnus) and the regional (Fagus) vegetation. From this level up to the top of the profile these two tree taxa contribute - together with Betula - always 50 to 80 % to the arboreal pollen sum. The upper 1.89 m of sediment of the Höllerer See core evidently date from the Subboreal and the Subatlantic. As Preboreal sediment was stated at the base of the profile it must be concluded that most of the Boreal and the Atlantic is - for whatever reason - not represented by sediment in this core. As no radiocarbon dates are available age estimates of the distinguished pollen zones can be achieved only by correlating major changes of the former vegetation with historical events which probably influenced the then contemporary vegetation. The pollen grains of the Triticum and Hordeum type found in samples of zone 2.1 might indicate the growing of cereals in the region during the Late Bronze Age. The first pollen grains of Secale date from the boundary Hallstatt/Latène Age (zone 2.2). The cereal curves become continuous in Bavarian times (Bajuwarenzeit, Middle Ages, zone 3.3). The Plantago laceolata curve, continuous since 1.7 m depth (zone 2.1), points to animal breeding since the Early Subatlantic (Hallstattzeit). This curve reaches its absolute maximum in Roman time (zone 3.1). Roman time forest clearance caused a drastic decrease of tree pollen curves (start of zone 3.1). Values of anthropogenic indicators as high as in zone 3.1 are found again - after a distinct decrease in zone 3.2 - not till the Bavarians settled in the region (6th century). Maximal Fagus values and the simultaneous total lack of anthropogenic indicators mark the Migration Period (zone 3.2). The Younger Subatlantic (zone 4) is characterized by a decrease of deciduous forests due to medieval forest clearance. At the same time the conifers Pinus and Picea gained in importance. The lake was probably used for retting hemp in Medieval times. The distinction of the pollen grains of Cannabis and Humulus might not be certain in all cases. It is known that hemp as well as hop was cultivated in the study area. Markers were added to the samples at the beginning of pollen preparation (13500 Lycopodium spores, sample volume 0.5 cm**3) and counted together with the pollen grains. Therefore pollen concentrations can be calculated: Concentration = C * F / V (with C = number of grains of a particular pollen type, V = volume of the untreated pollen sample, F = marker added/marker counted). F ranges from 39 to 1688. Factors that large are not suited to produce reliably interpretable pollen concentrations. Consequently no use was made of the pollen concentrations in this thesis, although a concentration diagram is added.

Sermon notes compiled by Solomon Prentice, 1724-1726

Leather top-bound volume containing notes kept by Solomon Prentice on sermons he attended between April 1724 and December 17, 1726, while he was an undergraduate at Harvard College. The volume contains one-to-two page entries on specific sermons and provides the biblical text and related questions and conclusions.

Sermon on redemption by David Tappan, 1781

Sewn notebook containing a forty-six page handwritten sermon composed by David Tappan based on the Biblical text Isaiah 65: 17, 18 and the subject of redemption. Tappan delivered the sermon multiple times as evidenced by the note on the first page, "March 11, 18, 25 Spring April 1781 Frisbee July 1782, Byfield July 1783, Lynn, Kimball. Dr. Huntington, Deerfield, French, Merrill, Dana."

Plate with King Hunting Rams

Metalwork, Iran, Sasanian; 1 13/16 in. x 8 5/8 in.; silver, mercury gilding, niello inlay

Applique in the shape of a lion's head

Albert Bierstadt; 2 1/64 in.x 2 23/64 in.; gold

Johannes von Gaza und Paulus Silentiarius: Kunstbeschreibungen Justinianischer Zeit,

Mode of access: Internet.

Wall decoration with geometric and floral decoration

1 ft. 1 1/2 in.x 1 ft. 11 1/2 in.; stucco

La Pointe Saint Mathieu, Brittany, France

The "Pointe Saint Mathieu" is one of the most westerly continental landmarks of France. The promontory is located at the entrance of the "Goulet de la Rade de Brest", that is the entrance channel of the harbour of Brest in Brittany (France). It marks also the Southern end of the "Chenal du Four" that is the main navigation channel between the islands of Ouessant, Molène and Béniquet, and Brittany. The "Chenal du Four" is reputed for its dangers. The tidal range is greater than 7 m in spring tides, and the mid-tide current may exceed 5 knots. The Saint Mathieu promontory is equipped with a lighthouse and a semaphore. The former is located in the ruins of an old monastery, founded during the 6th century AD by Saint Tanguy. The present ruins are the remnants of buildings from the 11th to 15th centuries. The first lighthouse was installed in 1689, although the monks of the monastery used to maintain a signal light since the 1250s. Completed in 1835, the present "Phare de la Pointe Saint-Mathieu" is 37 m high and it reaches 58.8 m above sea level During World War 2, the Pointe Saint Mathieu was defended by a series of concrete fortifications built by the Germans. Some were based upon some earlier French bunker systems, like the coastal battery at the Rospects which included 4 main gun bunkers (4*150 mm, or 2*150 mm & 2*105 mm), an observation bunker on the Western side close to sea, and several smaller structures. There was also the large Kéringar Blockhaus system, near Lochrist, located about 1 km inland and designed for 4 guns of 280 mm. Its command bunker remains a landmark along the main road. All this area was very-heavily bombed between 1943 and 1944, and particularly during the battle of Brest in August-September 1944 ("L'Enfer de Brest").

Molist, N. (ed.). La intervenció al sector 01 del Conjunt Històric d'Olèrdola. De la prehistòria a l'etapa romana (campanyes 1995-2006). Monografies d'Olèrdola, 2.

En muchas ocasiones, el conocimiento y la importancia de los grandes yacimientos arqueológicos son dos conceptos diferentes. La adecuación museográfica y las referencias específicas a materiales o intervenciones puntuales pueden enmascarar el valor real de los datos científicos que se conocen sobre ellos, limitando así su importancia dentro del conjunto de la información necesaria para la realización de síntesis y el conocimiento exhaustivo de un período histórico. En muchos casos, se añade la prolongación en el tiempo de excavaciones e intervenciones de consolidación cuyos resultados tardan en ser publicados o bien no llegan nunca a ver la luz, por lo que permanecen en los intrincados vericuetos del circuito científico, quedando como referencias de transmisión personal y provocando innecesarios vacíos en el conocimiento.

Nuevos elementos escultóricos del recinto de culto del Concilium Provinciae Hispaniae Citerioris (Tarraco, Hispania Citerior)

The work of the Director Plan for the Cathedral of Tarragona has allowed us to make a revision regarding the knowledge, chronology and features of the sacred area of the Concilium Provinciae Hispaniae Citerioris. We present diverse elements of architectural and sculptured decoration recovered from constructive levels of 1st century A.D, and the 6th century A.D levels of re-use and transformation, in contemporary constructions. All these elements ratify the process of imitation of the Forum Augustum made in the capital of the Hispania Citerior.

El territorio y la ciudad de Tarraco

This paper presents a brief description of the archaeological research in the territory and in the city of Tarraco, the ancient capital of provincia Hispania Tarraconensis and one of the main centres for the spread of Hispanic Christianity. Althoug Tarraco was the last capital under imperial control and the firs Hispanic metropolitan see, the city had only a secondary role by comparison with other Hispanic cities during late antiquity. This evolution shaped the development of Tarraco during the 7th century, but archaeologists identify an important architectural vitality still in the 6th century at the same time as other episcopal cities were evolving. During this period, the final Christianization of the symbolic spaces of ancient paganism took place, establishing the ideological basis of medieval urbanism that is still preserved today. The paper also interprets the sites through raising key questions as well as describing rural settlements, where archaeological knowledge is not so far advanced, due in part to the difficult nature of archaeological research, and in part to the need to study new construcitve models, as well as to the systematic collection of the relevant material culture.

Cassiodore, Variae, Livre 11 : traduction et commentaire historique

Ce mémoire est une traduction et un commentaire historique du livre 11 des Variae de Cassiodore concernant la période où il occupait le poste de préfet du prétoire (533-537). Si les Variae sont de la première importance comme sources pour l’Italie ostrogothique, cela ne se reflète malheureusement pas encore dans l’accessibilité du texte, qui n’a pas encore fait l’objet d’une traduction française ou d’un commentaire historique complet, d’où la nécessité de ce mémoire. On possède en effet peu de sources aussi pertinentes pour le VIe siècle en Italie, et ce qu’on sait par ailleurs sur l’administration de l’époque provient de sources éloignées géographiquement ou chronologiquement. Un commentaire de ce livre nous permet donc de dresser un bon portrait du préfet du prétoire et de son office ainsi que de la situation en Italie entre les années 530 et 540.