Tennyson had an enduring interest in geology, which has long been known by students and scholars of literary studies. As part of a broad introduction to nineteenth-century literature, students routinely study In Memoriamâs âgeological stanzasâ as evidence of both Tennysonâs engagement with geology and its significance for Victorian religious belief; those âdreadful hammersâ of which Ruskin complained.1 The role played by geology in Tennysonâs poetic imaginationâtaking In Memoriam as the usual exampleâhas had much attention. Excavated dinosaur fossils recovered from âscarped cliff and quarried stoneâ reveal how âNatureâ âcare[s] for nothingâ, while the âhillsâ that are âshadowsâ and that âflow / From form to formâ demonstrate Tennysonâs knowledge of contemporary ideas of geomorphology and specifically the uniformitarianism expounded by Charles Lyell in his Principles of Geology (1830â1833). Tennysonâs knowledge of Lyellâs Principles and its significance for his poetic thinking has been documented by literary critics for at least the past sixty years.2 However, Lyellâs geology, and geology generally, has nearly always been read in conjunction with In Memoriam (1851), and in consequence, the extent to which it figures in other poems has not yet been fully appreciated. This study examines Tennysonâs treatment of geology over an extended period across his three major mid-century poems, The Princess (1847), In Memoriam and Maud (1855). It argues that Tennysonâs poetics specifically and consistently engaged with geological patterns of thinking, theories and ideas in and around geological time and the reading of fossil remains . When Tennysonâs three poems are read together, this book claims, they can be seen to cohere in striking ways. One reason why the extent of the geology has not been fully appreciated is that it operates not only at the level of idea, image and metaphor but also at structural levels, and as deep structure it works powerfully but largely imperceptibly. Just as the earth itself âprovides the fabric on which all experience is locatedâ, geological structures and patterns of change order the internal logic of the poems, shaping the poetic expression and dictating the ways in which the drama of each poem unfolds.
Alongside Tennysonâs poems, this book also pays close attention to Lyellâs Principles of Geology as an understanding of Lyellâs text is crucial to an appreciation of the poetics of In Memoriam and Maud . However, debates in and around the works of other writers, geologists, polymaths and comparative anatomists, such as William Whewell, Hugh Miller , William Buckland , Adam Sedgwick , Gideon Mantell , Robert Chambers, Richard Owen and Richard Chenevix Trench also figure in readings of the poems, and an awareness of Tennysonâs understanding of the ideas of these writers and theorists modifies and enhances the perception of how and why Lyellian geology was so important to Tennysonâs poetic thinking.3 Chapter 2, for example, argues that Hugh Millerâs much-neglected (in terms of Tennysonâs writing) The Old Red Sandstone (1841) was seminal for Tennysonâs geological thinking and that it figures significantly in The Princessâs validation of contemporary gender ideologies. The less certain ideological territory of In Memoriam and Maud indicates the move away from the firmly theological epistemological grounds of Millerâs geology to the shifting landscape of Lyellâs Principles and its âuniformitarianâ vision of change. Thus, The Princess , In Memoriam and Maud can be seen to plot an increasingly radical movement from the geological and ideological confidence of The Princess, to In Memoriamâs Lyellian expression of doubt and division, and on to the geologically initiated crisis in language and meaning that characterises Maud.
Tennysonâs engagement with geology demonstrates the significance of geological language and ideas for the period, while it also illuminates the importance of poetic language in explicating the meanings and implications of geological discoveries for mid-nineteenth century thinking in philosophy, theology, and specifically for this study, for theories of the origin and nature of language. Thus, close attention to the poems and contemporary geological discourses not only enriches the understanding of Tennysonâs work but also adds to the understanding of the significance of early geological science for the nineteenth century and beyond. Crucially, a close examination of Tennyson and geology also offers a remarkable insight into the origins of the bifurcation of literature and science and the emergence of science writing as a distinctly separate form, as the poems chart a crisis in the assumption of the seamlessness of literary and scientific ways of knowing. In this, the poems are important not solely as aesthetic productions or as texts read within their contexts but as sites of experimentation and creativity where new geological thinking finds its wider significance and where new forms of knowing and experiencing are forged. While the focus of this study is mainly on the poetry, the geological texts are, of course, equally important in understanding this bifurcation. Reading the poetry and the geology together, the study argues, shows how they map a vital cultural shift in the history of the development of modern epistemologies.
There has been much exciting academic activity in the field of nineteenth-century literature and science in the last decade. In the area of poetry and science, there have been a number of seminal studies (Holmes 2009; Tate 2012; Brown 2013) and also in nineteenth-century literature and geology (OâConnor 2007; Buckland 2013).4 Most scholarship, however, has taken an historicist approach, while Noah Heringmanâs nuanced study of Romantic poetry and geology, Romantic Rocks, Aesthetic Geology (2004), stands out as offering a theoretically inflected approach that addresses the origins of Romantic ways of knowing and persuasively argues that Romanticism and geology both âspring from a common source, landscape aestheticsâ.5 The approach to Tennysonâs poems and geology in this book makes use of a range of literary critical practices, combining historical contextualisation with close readings, but also drawing on modern literary theory and specifically Mikhail Bakhtinâs model of dialogism . Theory, however, is not merely projected back onto the nineteenth-century texts as a way of understanding them via new paradigms. Rather, it is there to demonstrate the part that these poetic and geologic texts played in originating modern theory itself. Thus, one of the broadest arguments of this book is that a close examination of these texts adds to the understanding of the formation of modern critical thinking and specifically early twentieth-century language theory, as will be discussed.
This introductory first chapter begins by discussing some of the issues concerning reading literature and science together. It looks briefly at the âtwo culturesâ debate and at how the texts here studiedâpoetic and geologicalâare seminal themselves in the development of what we now think of as âtwo culturesâ. As the connections between geology and contemporary language theory are important for the bookâs larger argument, the introduction outlines the crucial concepts and debates around language that the texts were part of. Following this, it sets in place some of the ideas involved in reading âremainsââgeological or otherwiseâin Tennysonâs poems. Finally, as a preamble to Chap. 2âs analysis of The Princess , Hugh Millerâs The Old Red Sandstone (1841) is examined as Millerâs popular theologically orientated geology figures prominently in The Princess , and an understanding of how it operates in the poem helps to bring into relief the heterodoxy of Lyellâs geology.
Tennyson, Literature and Science
Studying literature and science at a time when these categories are being founded raises many issues concerning their relationship. As Gillian Beer demonstrated (1983, 1996) the flow of ideas between literature and science is not a âone-way trafficâ; literature does not âact as a mediator for a topic (science) that precedes it and that remains intact after its re-presentationâ. Rather, âScientific and literary discourses overlapâ albeit âunstablyâ. Beer draws attention to the way ideas shape and re-shape themselves as they move through discourses, and in turn, shape and re-shape human thought, suggesting, much âis to be gained from analysing the transformations that occur when ideas change creative context and encounter fresh readersâ.6 Beerâs ground-breaking work is still producing fresh insights and how nineteenth-century literature and science relate to each other is still a critical issue in itself.
Ralph OâConnorâs extensive examination of geology, poetry and the scientific imagination, The Earth on Show: Fossils and the Poetics of Popular Science, 1802â1856 (2007), makes a number of critical points about how literature and science might be read together. One of his aims is to address what he sees as a bias in literary criticism towards the literary text as the central form worthy of analysis. What he calls âthe âpoet x and science yâ frameworkâ, in which âLiterature represents the centre and science one of several possible peripheries, supplying the raw material for poetic productionâ. OâConnor offers the title of Dennis R. Deanâs meticulous study of Tennysonâs geological sources, Tennyson and Geology, as one example of what the x y framework tends to look like.7 The present work, of course, is exactly that tooâTennyson and Geologyâand the focus of this book is, mainly, the poetic texts. However, this study moves beyond the formula OâConnor discusses. The geologic texts are not seen as peripheral, nor as merely the source of poetic embellishment. Rather, one of the aims of this study is to apply to all texts, poetic and geologic, the same level of literary critical awareness. Thus, Chap. 3 scrutinises Lyellâs Principles with the same attention to literary and rhetorical device as given to Tennysonâs poems. But the study also aims to examine the ways in which the poetry interrogates the use of literary device in Lyellâs geological text. Tennysonâs reading of geology produced poems that were not merely passive receptacles of geological ideas, just as geological discourses were not merely sources for new metaphors. The poems test out the fitness of geological concepts, processes and patterns of change by probing the logic and intelligence of the metaphoric structuring used by those writing about geology, and in doing so they extend and develop the meaning of geology. They do not merely record particular intellectual shifts occurring in the period or document the cultural assimilation of things happening in geology. The poetry played a role in giving geology cultural meaning while it also helped explain geology to itself.
OâConnor also usefully questions the assumption that the âperiod between 1780 and 1820â saw a âwatershedâ in the relationship between literature and science âculminating in a divorceâ. Rather, OâConnor argues for the âglacial slowness of this metamorphosisâ, which, by 1820 âhad hardly begunâ. For this reason, he argues, âwe need to stop thinking in terms of âgivenâ dichotomies such as âscience and literary writingsââ, as âfor at least the first two-thirds of the nineteenth century, this distinction cannot be assumedâ.8 Thus, as the specific set of value systems that created our pr...