Nohajenelābadhinjo : manuscript, 1870?

Foreign paper, watermark: Dorling Gregory, London, 1869.

Dhoā:gajal:arasī : manuscript, 1890?

Foreign wove paper; watermark: Munro, 1883.

Muṛbadhno ek āćhoḍo (?) : manuscript, 1900 ?

Foreign paper, manufactured in Bombay by Abdoola Saheb Abdool Rehman Hurufullah, watermark : "River Jumna".

Pāñḍavānī saṇgāroṇī : manuscript, 1900?

Local paper.

[ Ghaṭpāṭjī dhoā]

Prayers to be recited during the ghaṭpāṭ ceremony; prayer includes recitation of the name of Ismāʻīlī Imāms as well as those of Pīrs.

Tarjamah-ʹi Tārīkh-i Yangī Dunyā : manuscript, 18th cent

Title supplied by the cataloger.

Kitāb ʻAjāyib al-makhlūqāt wa-gharāyib al-mawjūdāt : manuscript, [circa 1650-1700]

On wonders of creation.

Rawda al-Ushshaq (Garden of Lovers) of Arifi, with three paintings : manuscript, ca. 1560-1575

Artist unknown.

Manuscript of a Divan of Hafiz : manuscript, ca. 1527

Artist unknown.

The Court of Justice of the European Union. College of Europe Research Paper in Law 02/2014

The Court of Justice of the European Union is one of the institutions of the Union. Praised by some as the relentless and steady motor of European integration and attacked by others as an example of a clearly biased institution, more ink has perhaps been spilled over the years on discussing the (de)merits of the Court of Justice than any other Union institution. In face of such considerable literature coming from legal, political science, sociological, and more recently also historical quarters, this chapter cannot but scratch the surface of the vast topic by providing a concise introduction into selected institutional themes in a legal1 and, where possible, diachronic perspective: the structure of the Union courts located in Luxembourg; basic information about the type of judicial business the Court of Justice carries out; the composition of the Court of Justice, including the recent changes made to the way in which judges and advocates-general are selected; the often discussed style and structure of the judgments; and, finally, the even more frequently discussed and recurring question of the legitimacy of the Court of Justice.

Distribution of basalt boulders and ice rafted debris in the region of the Iceland-Faroe-Ridge (Fig. 6-12)

Psephitic particles in the region of the Iceland-Faeroe-Ridge have been transported and deposited by means of a complex interplay of glacier movements and drifting icebergs. The composition of the particle association is controlled by the sedimentation of basaltic rock particles derived from the ridge itself and, in addition to that and in southern parts of the ridge, from the Faeroe Islands, the Faeroe-Bank and the Bill Baileys-Bank. Besides, there are crystalline and sedimentary dropstones showing a very varied petrography and a wide range of particle sizes. Their percentage becomes greater as the distance from the ridge increases. The association of dropstones is relatively homogeneous in the region of the ridge and only at greater distances from the ridge it becomes more differentiated. Owing to their composition and distribution, as well as on the basis of characteristic fossils and rock types, the drop-stones are derived from Scandianvia and Great Britain. During periods of maximum glaciation, the Icland-Faeroe-Ridge, th eFaeroe-Bank and the Bill Baileys-Bank were under ice.

Los estetas de Teópolis : novela /

RBC: "Juan Como Pascual Barcelona"--Stamp on half t.p.