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Additional volcanic flows downhill from the vent are visible in the second-epoch images, although we cannot rule out that they were present but invisible in the first epoch because of differences in imaging geometry. We interpret these results as evidence of ongoing volcanic activity on Venus.<\/jats:p>","DOI":"10.1126\/science.abm7735","type":"journal-article","created":{"date-parts":[[2023,3,15]],"date-time":"2023-03-15T14:00:09Z","timestamp":1678888809000},"page":"1205-1208","update-policy":"https:\/\/doi.org\/10.34133\/aaas_crossmark","source":"Crossref","is-referenced-by-count":96,"title":["Surface changes observed on a Venusian volcano during the Magellan mission"],"prefix":"10.1126","volume":"379","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-0974-6293","authenticated-orcid":true,"given":"Robert R.","family":"Herrick","sequence":"first","affiliation":[{"name":"Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK 99775, USA."}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-8846-2175","authenticated-orcid":true,"given":"Scott","family":"Hensley","sequence":"additional","affiliation":[{"name":"Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA."}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"221","reference":[{"key":"e_1_3_2_2_2","unstructured":"V. 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