Formation of lobate debris aprons on Mars: Assessment of regional ice sheet collapse and debris-cover armoring
Lobate debris aprons (LDA) are lobate-shaped aprons surrounding scarps and isolated
massifs that are concentrated in the vicinity of the northern Dichotomy Boundary on Mars …
massifs that are concentrated in the vicinity of the northern Dichotomy Boundary on Mars …
Amazonian mid-to high-latitude glaciation on Mars: Supply-limited ice sources, ice accumulation patterns, and concentric crater fill glacial flow and ice sequestration
JL Fastook, JW Head - Planetary and Space Science, 2014 - Elsevier
Concentric crater fill (CCF) occurs in the interior of impact craters in mid-to high latitudes on
Mars and is interpreted to have formed by glacial ice flow and debris covering. We use the …
Mars and is interpreted to have formed by glacial ice flow and debris covering. We use the …
Cold‐based debris‐covered glaciers: Evaluating their potential as climate archives through studies of ground‐penetrating radar and surface morphology
We describe the morphology and internal structure of Mullins and Friedman Glaciers, two
cold‐based, debris‐covered alpine glaciers that occur in neighboring valleys in the …
cold‐based, debris‐covered alpine glaciers that occur in neighboring valleys in the …
Evidence for Amazonian northern mid-latitude regional glacial landsystems on Mars: Glacial flow models using GCM-driven climate results and comparisons to …
JL Fastook, JW Head, F Forget, JB Madeleine… - Icarus, 2011 - Elsevier
A fretted valley system on Mars located at the northern mid-latitude dichotomy boundary
contains lineated valley fill (LVF) with extensive flow-like features interpreted to be glacial in …
contains lineated valley fill (LVF) with extensive flow-like features interpreted to be glacial in …
Preservation of Late Amazonian Mars ice and water-related deposits in a unique crater environment in Noachis Terra: Age relationships between lobate debris …
GA Morgan, JW Head, DR Marchant - Icarus, 2011 - Elsevier
The Amazonian period of Mars has been described as static, cold, and dry. Recent analysis
of high-resolution imagery of equatorial and mid-latitude regions has revealed an array of …
of high-resolution imagery of equatorial and mid-latitude regions has revealed an array of …
Modeling concentric crater fill in Utopia Planitia, Mars, with an ice flow line model
Impact craters in the mid-latitudes of Mars are commonly filled to variable degrees with some
combination of ice, dust, and rocky debris. Concentric surface features visible in these …
combination of ice, dust, and rocky debris. Concentric surface features visible in these …
Age, origin and evolution of Antarctic debris-covered glaciers: Implications for landscape evolution and long-term climate change
SL Mackay - 2016 - search.proquest.com
Antarctic debris-covered glaciers are potential archives of long-term climate change.
However, the geomorphic response of these systems to climate forcing is not well …
However, the geomorphic response of these systems to climate forcing is not well …