- 10th century castle, on its mound, with a wooden palisade enclosure
- A Bishop
- A domed church
- A juggler, after a miniature
- According to Viollet-le-Duc
- An 11th century knight, after the Bayeux tapestry
- An attempt to restore the Krak, according to M. Rey
- Anglo-Norman knight, after a tomb from 1277
- Bathynomus giganteus
- Bathyteuthis abyssicola
- Bentheuphausia amblyops, from 1,000 fathoms
- Bronze Cat
- Bust of Francesco Foscari
- Byzantine Crosses—Campo S. Maria Mater Domini
- Byzantine enamels from the Limburg reliquary
- Byzantine Relief from South Side, S. Marco
- Capitals, Atrium, S. Marco
- Ca’ d’Oro
- Cloister of S. Francesca della Vigna
- Collosendeis arcuatus, from a depth of 1,500 metres
- Columns of SS. Mark and Theodore
- Crown of Charlemagne, kept in the imperial treasury of Vienna
- Divider
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Divider - Divider
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- Doge’s Palace—Sala del Maggior Consiglio
- Doge’s Palace—The Cortile
- Doge’s Palace—The Judgment of Solomon Corner
- Doorway with Coloured Relief of SS. Mark and Anianus
- Egyptian jewellery of the XIXTH dynasty
- Emperor Anastasius in consular costume
- Emperor Justinian and his court - Mosaic of San Vitale, in Ravenna
- Emperor Lothaire
- Emperor Otton III, after a miniature from the Evangelist of Bamberg
- Empress Theodora
- Enamelled copper stock. The Annunciation. Limoges, 13th century
- Enamelled copper vase by G. Alpaïs de Limoges
- Euphausia latifrons, from the surface of the sea
- Fishing Boats
- Fishing Boats on the Giudecca
- Former Constantinian Basilica of Saint Peter. Restitution
- Gautier Bardins, bailiff and adviser to the king in the 13th century, according to his tombstone
- Geoffroy Plantagenet
- Germanic costume (5th-8th century)
- Globigerina ooze
The Globigerina ooze is perhaps the best known of all the different deep-sea deposits. It was discovered and first described by the officers of the American Coast Survey in 1853. It is found in great abundance in the Atlantic Ocean in regions shallower than 2,200 fathoms. Deeper than this, it gradually merges into the ‘Red mud.’ It is mainly composed of the shells of Foraminifera, and of these the different species of Globigerina are the most abundant. It is probably formed partly by the shells of the dead Foraminifera that actually live on the bottom of the ocean and partly by the shells of those that live near the surface or in intermediate depths and fall to the bottom when their lives are done. So abundant are the shells of these Protozoa that nearly 95 per cent. of the Globigerina ooze is composed of carbonate of lime. The remaining five per cent. is composed of sulphate and phosphate of lime, carbonate of ammonia, the oxides of iron and manganese, and argillaceous matters. The oxides of iron and manganese are probably of meteoric origin; the argillaceous matter may be due to the trituration of lumps of pumice stone and to the deposits caused by dust storms. - Gold pectoral inlaid with enamel
- Grand Canal, with the Riva del Carbon and Rialto Bridge
- Hypobythius calycodes
- Interior facade of the old St. Peter's Church in the Vatican
- Knight of around 1220, from the Villard de Honnecour album
- La Ziza, palace of the Norman and Swabian kings of Sicily, near Palermo
- Melanocetus Murrayi, 1,850–2,450 fathoms
- Murano