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University of Pennsylvania

A Melting Fossil: Constituting Planetary Time In The Cryosphere, 1815-1980

Abstract

dc:description.abstract

A Melting Fossil traces how, since the nineteenth century, naturalists and scientists have used ice as a natural chronometer to understand the deep past and future of the Earth. Using archival sources that span two centuries and three continents, this project argues that through ice, Earth scientists have refashioned their conceptualization of deep time from something slow, lumbering, and uniform to something much more capricious—a shift that has profoundly shaped social understandings of environmental change. By tracing how scientific assertions about temporality have materialized, and how this materialization determines (and limits) cultural notions of and political actions on the past and future of the planet, A Melting Fossil reveals how deep time has expanded beyond the purview of the Earth sciences to form an epistemological frame for human-environment relationships.

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Rider, Alexis
Advisor dc:contributor.advisor
  • Etienne S. Benson

Rights

dc:rights
Statement dc:rights
  • Alexis Rider
Language dc:language
en

Identifiers

dc:identifier.*
Repository record dc:identifier.uri
https://repository.upenn.edu/handle/20.500.14332/32117
OAI identifier oai:identifier
oai:repository.upenn.edu:20.500.14332/32117

Chain of custody

source
Harvested from
University of Pennsylvania
Base URL
repository.upenn.edu/server/oai/request
Last updated
2026-07-24
Source record
OAI-PMH GetRecord
related terms
citation

Rider, Alexis. A Melting Fossil: Constituting Planetary Time In The Cryosphere, 1815-1980. 2022. https://repository.upenn.edu/handle/20.500.14332/32117