Skip to Main Content
Skip Nav Destination
GEOREF RECORD

Geomorphologic observations and physical hypothesis on Martian gullies

Adriano Nardi and Antonio Piersanti
Geomorphologic observations and physical hypothesis on Martian gullies
Italian Journal of Geosciences (June 2022) 141 (2): 245-258

Abstract

We propose a hypothesis to explain the erosive phenomenon of Martian gullies under current climatic conditions. This model is consistent with the morphology and finds support in the characteristic geographic diffusion of the gullies, which seem to avoid exposure to the sun and the hottest latitudes. We hypothesize a transient flow of spring water fed by melting permafrost which can occur only in certain latitudes and altitudes, with seasonal variability and for a very short time. Furthermore, this phenomenon can only occur in certain ranges of temperature and pressure, therefore when particular and sporadic weather conditions allow it. For this reason, we propose to call it weather-springing water (WSW).


ISSN: 2038-1719
EISSN: 2038-1727
Coden: BOGIAT
Serial Title: Italian Journal of Geosciences
Serial Volume: 141
Serial Issue: 2
Title: Geomorphologic observations and physical hypothesis on Martian gullies
Affiliation: Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
Pages: 245-258
Published: 202206
Text Language: English
Publisher: Societa Geologica Italiana, Rome, Italy
References: 64
Accession Number: 2022-048189
Categories: Extraterrestrial geology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 2 tables, sect.
Country of Publication: Italy
Secondary Affiliation: GeoRef, Copyright 2023, American Geosciences Institute. Abstract, Copyright, Societa Geologica Italiana. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 202236
Close Modal

or Create an Account

Close Modal
Close Modal