How We Read the Earth: Geological Principles for Reconstructing the History of the Planet
DOI:
https://doi.org/10.22201/ceide.16076079e.2026.27.3.6Keywords:
Historical geology, Stratigraphy, Geological time, Geological recordAbstract
How can Earth’s history be reconstructed from scattered rocks and fossils? This article explores how geological principles allow scientists to read the geological record and interpret the evolution of the planet. Through a narrative approach, concepts such as superposition, original horizontality, lateral continuity, faunal succession, uniformitarian reasoning, and inclusion and cross-cutting relationships are presented as tools for ordering events, recognizing transformations, and reconstructing past environments. Formulated between the seventeenth and nineteenth centuries, these principles remain essential to modern geological interpretation and theories such as plate tectonics. Beyond their technical value, they represent a way of building knowledge grounded in observation, comparison, and reasoning from natural evidence.
References
Cartwright, M. (2023). Scientific revolution. World History Encyclopedia. https://www.worldhistory.org/Scientific_Revolution/.
Celâl Şengör, A. M. (2021). History of geology. En Encyclopedia of geology (2.ª ed., pp. 1–36). https://doi.org/10.1016/B978-0-08-102908-4.00084-9.
Eyles, V. (1947). James Hutton (1726–1797) and Sir Charles Lyell (1797–1875). Nature, 160, 694–695. https://doi.org/10.1038/160694a0.
Genske, D. D. (2024). Geological principles. En Engineering geology (pp. 5-43). Springer Textbooks in Earth Sciences, Geography and Environment. Springer. https://doi.org/10.1007/978-3-662-68762-8_2.
Hepburn, B., y Hanne, A. (2021). Scientific method. En E. N. Zalta (Ed.), The Stanford encyclopedia of philosophy (ed. de verano de 2021). https://plato.stanford.edu/archives/sum2021/entries/scientific-method/.
Lyell, C. (2009). Principles of geology: An attempt to explain the former changes of the Earth’s surface, by reference to causes now in operation. Cambridge University Press. https://doi.org/10.1017/CBO9780511701559 (Obra original publicada en 1830)
Paola, C., Ganti, V., Mohrig, D., Runkel, A., y Straub, K. M. (2018). Time not our time: Physical controls on the preservation and measurement of geologic time. Annual Review of Earth and Planetary Sciences, 46, 409–438. https://doi.org/10.1146/annurev-earth-082517-010129.
Qian, S.-P., Gazel, E., y Wang, J.-H. (2025). Mantle transition zone water triggers lithospheric weakening and spreading. Geology, 53(5), 461–466. https://doi.org/10.1130/G52804.1.
Smithsonian National Museum of Natural History. (s. f.). Homepage. https://naturalhistory.si.edu/.
The Geological Society. (s. f.). Plate tectonics. https://www.geolsoc.org.uk/Plate-Tectonics.html.
University of California Museum of Paleontology. (s. f.). Nicholas Steno (1638–1686). Understanding Evolution. https://ucmp.berkeley.edu/history/steno.html.
Zhan, R., Harper, D. A. T., Jin, J., Liang, Y., Liu, J., Stemmerik, L., y Stouge, S. (2014). Middle Ordovician Aporthophyla brachiopod fauna from the roof of the world, southern Tibet. Palaeontology, 57(1), 141–170. https://doi.org/10.1111/pala.12058.
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