The Modernity of la Mode: a History of the French Revolution Through the Lens of Fashion, Culture, and Identity

In my thesis, I explore the cultural history of the French Revolution and its relation to the modern era which ensued. Many historians have studied the French Revolution as it relates to culture, the rise of modernity, and fashion. I combine the unique histories of all three of these aspects to reach an understanding of the history of the French Revolution and fashion’s role in bringing about change. In the majority of literature of costume history, discussion of fashion surrounds its reflective properties. Many historians conclude fashion as a reflection of the broader cultural shifts that occurred during the Revolution. I, on the other hand, propose that fashion is an active force in bringing out cultural change during this time. In exploring fashion as a historical motivator, I examine the aesthetic world of fashion from 1740 to 1815, the modern system of cultural dissemination of fashion through particular historical heroes, and the rise of “taste” and its relation to modern identity. Through aesthetics, culture, and identity, I argue that fashion is a decisive force of culture in that it creates a visual world through which ideas form and communicate.

Eugene Onegin As A Bridge Between Worlds: Aleksandr Pushkin As Translator Of The 19Th-Century Russian Experience

In my thesis, I use literary criticism, knowledge of Russian, and elements of translation theory to study the seminal poet of the Russian literary tradition ¿ Aleksandr Pushkin. In his most famous work, Eugene Onegin, Pushkin explores the cultural and linguistic divide in place at the turn of the 19th century in Russia. Pushkin stands on the peripheries of several colliding worlds; never fully committing to any of them, he acts as a translator between various realms of the 19th-century Russian experience. Through his narrator, he adeptly occupies the voices, styles, and modes of expression of various characters, displaying competency in all realms of Russian life. In examining Tatiana, his heroine, the reader witnesses her development as analogous to the author¿s. At the center of the text stands the act of translation itself: as the narrator ¿translates¿ Tatiana¿s love letter from French to Russian, the author-narrator declares his function as a mediator, not only between languages, but also between cultures, literary canons, social classes, and identities. Tatiana, as both main character and the narrator¿s muse, emerges as the most complex figure in the novel, and her language manifests itself as the most direct and capable of sincerity in the novel. The elements of Russian folklore that are incorporated into her language speak to Pushkin¿s appreciation for the rich Russian folklore tradition. In his exaltation of language considered to be ¿common¿, ¿low¿ speech is juxtaposed with its lofty counterpart; along the way, he incorporates myriad foreign borrowings. An active creator of Russia¿s new literary language, Pushkin traverses linguistic boundaries to synthesize a fragmented Russia. In the process, he creates a work so thoroughly tied to language and entrenched in complex cultural traditions that many scholars have argued for its untranslatability.

Detrital Zircon Evidence for Mixing of Mazatzal Province Age Detritus With Yavapai Age (ca. 1700-1740 Ma) and Older Detritus in the ca. 1650 Ma Mazatzal Province of Central New Mexico, USA

Preliminary detrital zircon age distributions from Mazatzal crustal province quartzite and schist exposed in the Manzano Mountains and Pedernal Hills of central New Mexico are consistent with a mixture of detritus from Mazatzal age (ca. 1650 Ma), Yavapai age (ca. 1720 Ma.), and older sources. A quartzite sample from the Blue Springs Formation in the Manzano Mountains yielding 67 concordant grain analyses shows two dominant age peaks of 1737 Ma and 1791 Ma with a minimum peak age of 1652 Ma. Quartzite and micaceous quartzite samples from near Pedernal Peak give unimodal peak ages of ca. 1695 Ma and 1738 Ma with minimum detrital zircon ages of ca. 1625 Ma and 1680 Ma, respectively. A schist sample from the southern exposures of the Pedernal Hills area gives a unimodal peak age of 1680 Ma with a minimum age of ca. 1635 Ma. Minor amounts of older detritus (>1800 Ma) possibly reflect Trans-Hudson, Wyoming, Mojave Province, and older Archean sources and aid in locating potential source terrains for these detrital zircon. The Blue Springs Formation metarhyolite from near the top of the Proterozoic section in the Manzano Mountains yields 71 concordant grains that show a preliminary U-Pb zircon crystallization age of 1621 ¿ 5 Ma, which provides a minimum age constraint for deposition in the Manzano Mountains. Normalized probability plots from this study are similar to previously reported age distributions in the Burro and San Andres Mountains in southern New Mexico and suggest that Yavapai Province age detritus was deposited and intermingled with Mazatzal Province age detritus across much of the Mazatzal crustal province in New Mexico. This data shows that the tectonic evolution of southwestern Laurentia is associated with multiple orogenic events. Regional metamorphism and deformation in the area must postdate the Mazatzal Orogeny and ca. 1610 Ma ¿ 1620 Ma rhyolite crystallization and is attributed to the Mesoproterozoic ca. 1400 ¿ 1480 Ma Picuris Orogeny.