Title Information
Title
Cold-Climate (Periglacial) Landforms on the Earth and Mars: Geomorphic Evidence for Ice-Related Flow and Conditions for the Generation of Meltwater.
Name: Personal
Name Part
Morgan, Gareth A.
Role
Role Term: Text
creator
Origin Information
Copyright Date (keyDate="yes", encoding="w3cdtf")
2009
Physical Description
Extent
xxii, 326 p.
digitalOrigin
born digital
Note
Thesis (Ph.D.) -- Brown University (2009)
Name: Personal
Name Part
Head, James
Role
Role Term: Text
director
Name: Personal
Name Part
Pieters, Carle
Role
Role Term: Text
reader
Name: Personal
Name Part
Herbert, Timothy
Role
Role Term: Text
reader
Name: Personal
Name Part
Wyatt, Michael
Role
Role Term: Text
reader
Name: Personal
Name Part
Chicarro, Augustin
Role
Role Term: Text
reader
Name: Corporate
Name Part
Brown University. Geological Sciences
Role
Role Term: Text
sponsor
Genre (aat)
theses
Abstract
Under the current paradigm of Mars history, the planet is thought to have undergone a global climatic change, from relatively warm and wet conditions during the Noachian, to conditions during the Amazonian characterized by temperatures and pressures largely below the triple point of water. Analysis of high-resolution datasets have revealed an array of young landforms associated with both ice and liquid water at latitudes where it is currently unstable, suggesting that significant climatic change has also occurred during the post-Noachian. This thesis reports on the detailed morphological investigation, mapping and dating of Amazonian and Hesperian landforms indicative of the action of ice/water. This includes: gullies, previously unreported lobate debris tongues, large-scale lineated valley fill/lobate debris apron (LVF/LDA) deposits, and valley networks. Comparisons of these features of different ages permit an examination of the magnitude and extent of climatic change. To aid the interpretation of the landform assemblages, two field campaigns were undertaken in the Antarctic Dry Valleys. These have long been described as the most Mars-like terrestrial environment and are also an important focus of climate research on Earth due to their sensitivity. This has led to the development of a martian gully formation model based on the melting of windblown snowpacks under specific insolation conditions. This research indicates that multiple episodes of climate change have occurred on Mars resulting in the surficial deposition and evolution of ice, at both the regional scale in the form of debris-covered glaciers (LVF/LDA deposits), and within localized microclimate zones. The melting of surface ice has provided a source of water for the generation of fluvial activity. This appears to have occurred over the last several million years during periods of preferential insolation to form gullies, and during the Hesperian, in response to a large impact into glacial deposits, resulting in valley formation.
Subject (Local)
Topic
Mars
Subject (Local)
Topic
Gullies
Subject (Local)
Topic
Climate
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/940955")
Topic
Geomorphology
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/942975")
Topic
Glaciers
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/864281")
Topic
Climatology
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/1243063")
Geographic
Mars (Planet)
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/1239992")
Geographic
Antarctica
Record Information
Record Content Source (marcorg)
RPB
Record Creation Date (encoding="iso8601")
20091218
Language
Language Term: Code (ISO639-2B)
eng
Language Term: Text
English
Identifier: DOI
10.7301/Z0833Q9F
Access Condition: rights statement (href="http://rightsstatements.org/vocab/InC/1.0/")
In Copyright
Access Condition: restriction on access
Collection is open for research.
Type of Resource (primo)
dissertations