Hit papers significantly outperform the citation benchmark for their cohort. A paper qualifies
if it has ≥500 total citations, achieves ≥1.5× the top-1% citation threshold for papers in the
same subfield and year (this is the minimum needed to enter the top 1%, not the average
within it), or reaches the top citation threshold in at least one of its specific research
topics.
Seasonal Flows on Warm Martian Slopes
2011354 citationsA. S. McEwen, L. Ojha et al.profile →
Peers — A (Enhanced Table)
Peers by citation overlap · career bar shows stage (early→late)
cites ·
hero ref
This map shows the geographic impact of C. M. Dundas's research. It shows the number of citations coming from papers published by authors working in each country. You can also color the map by specialization and compare the number of citations received by C. M. Dundas with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites C. M. Dundas more than expected).
This network shows the impact of papers produced by C. M. Dundas. Nodes represent research fields, and links connect fields that are likely to share authors. Colored nodes show fields that tend to cite the papers produced by C. M. Dundas. The network helps show where C. M. Dundas may publish in the future.
Co-authorship network of co-authors of C. M. Dundas
This figure shows the co-authorship network connecting the top 25 collaborators of C. M. Dundas.
A scholar is included among the top collaborators of C. M. Dundas based on the total number of
citations received by their joint publications. Widths of edges
represent the number of papers authors have co-authored together.
Node borders
signify the number of papers an author published with C. M. Dundas. C. M. Dundas is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Landis, M. E., A. S. McEwen, I. J. Daubar, et al.. (2020). South Polar Layered Deposits Near-Surface Properties Inferred from a Dated Impact Crater. LPICo. 2099. 6025.1 indexed citations
7.
Landis, M. E., S. Byrne, I. J. Daubar, K. E. Herkenhoff, & C. M. Dundas. (2017). Current Resurfacing Rate of the North Polar Layered Deposits, Mars. Lunar and Planetary Science Conference. 1588.1 indexed citations
8.
Milazzo, M. P., et al.. (2017). The Challenge for 2050: Cohesive Analysis of More than One Hundred Years of Planetary Data. LPICo. 1989. 8070.1 indexed citations
9.
Dundas, C. M., L. Keszthelyi, Christopher W. Hamilton, et al.. (2017). The Hydrothermal System of the 2014-2015 lava Flows at Holuhraun, Iceland: An Analog for Martian Lava-Water Interactions. Lunar and Planetary Science Conference. 2470.3 indexed citations
10.
Ostrach, L. R. & C. M. Dundas. (2017). Topographic Assessment of Hollows on Mercury: Distinguishing Among Formation Hypotheses. LPI. 1656.1 indexed citations
11.
Landis, M. E., S. Byrne, I. J. Daubar, K. E. Herkenhoff, & C. M. Dundas. (2016). Surface Age and Resurfacing Rates of the North Polar Layered Deposits, Mars. LPI. 1926(1903). 2154.1 indexed citations
12.
Chojnacki, M., et al.. (2015). Recurring Slope Lineae on Mars: Atmospheric Origin?. European Planetary Science Congress.9 indexed citations
13.
Keszthelyi, L., W. L. Jaeger, C. M. Dundas, & A. S. McEwen. (2014). A New Paradigm for, and Questions About, Volcanism on Mars. LPICo. 1791. 1189.4 indexed citations
14.
Jaeger, W. L., et al.. (2014). Evidence for Possible Mechanical Erosion by Lava at Athabasca Valles, Mars, from HiRISE and CTX Images and Topography. Lunar and Planetary Science Conference. 1683.5 indexed citations
15.
Ojha, L., A. S. McEwen, C. M. Dundas, et al.. (2011). Transient Slope Lineae on Mars: Observations by HiRISE. LPI. 2101.2 indexed citations
16.
Dundas, C. M., L. Keszthelyi, V. J. Bray, & A. S. McEwen. (2010). The Cratering Record of Young Platy-ridged Lava on Mars: Implications for Material Properties. Lunar and Planetary Science Conference. 2486.1 indexed citations
17.
Dundas, C. M., A. S. McEwen, S. Diniega, & Shane Byrne. (2009). New and Recent Gully Activity on Mars. AGU Fall Meeting Abstracts. 2009.1 indexed citations
18.
Dundas, C. M., et al.. (2007). Early HiRISE Observations of Fractured Mounds. Lunar and Planetary Science Conference. 2173.1 indexed citations
19.
Dundas, C. M., et al.. (2007). Initial HiRISE Observations of Cratered Cone Groups on Mars. LPI. 2116.6 indexed citations
20.
Weitz, C. M., et al.. (2007). Early HiRISE Observations of Light-toned Layered Deposits. LPI. 1442.2 indexed citations
Rankless uses publication and citation data sourced from OpenAlex, an open and comprehensive
bibliographic database. While OpenAlex provides broad and valuable coverage of the global
research landscape, it—like all bibliographic datasets—has inherent limitations. These include
incomplete records, variations in author disambiguation, differences in journal indexing, and
delays in data updates. As a result, some metrics and network relationships displayed in
Rankless may not fully capture the entirety of a scholar's output or impact.