110 results on '"Aileen Yingst"'
Search Results
102. Preface
- Author
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Aileen Yingst
- Subjects
General Medicine - Published
- 2011
103. Soil sedimentology at Gusev Crater from Columbia Memorial Station to Winter Haven
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R. Aileen Yingst, Jeffrey M. Moore, Christian Schröder, A. T. Knudson, C. d’Uston, Robert C. Anderson, Nathalie A. Cabrol, Ron Li, Catherine M. Weitz, Ronald Greeley, Edmond A. Grin, Kenneth E. Herkenhoff, Barbara A. Cohen, and Brenda J. Franklin
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Atmospheric Science ,Population ,Geochemistry ,Soil Science ,Mineralogy ,Aquatic Science ,Oceanography ,Texture (geology) ,Impact crater ,Geochemistry and Petrology ,Earth and Planetary Sciences (miscellaneous) ,Sedimentology ,Pebble ,education ,Earth-Surface Processes ,Water Science and Technology ,Martian ,geography ,education.field_of_study ,geography.geographical_feature_category ,Ecology ,Paleontology ,Forestry ,Geophysics ,Volcano ,Space and Planetary Science ,Aeolian processes ,Geology - Abstract
[1] A total of 3140 individual particles were examined in 31 soils along Spirit's traverse. Their size, shape, and texture were quantified and classified. They represent a unique record of 3 years of sedimentologic exploration from landing to sol 1085 covering the Plains Unit to Winter Haven where Spirit spent the Martian winter of 2006. Samples in the Plains Unit and Columbia Hills appear as reflecting contrasting textural domains. One is heterogeneous, with a continuum of angular-to-round particles of fine sand to pebble sizes that are generally dust covered and locally cemented in place. The second shows the effect of a dominant and ongoing dynamic aeolian process that redistributes a uniform population of medium-size sand. The texture of particles observed in the samples at Gusev Crater results from volcanic, aeolian, impact, and water-related processes.
- Published
- 2008
104. Quantitative morphology of rocks at the Mars Pathfinder landing site
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Albert F. C. Haldemann, R. Aileen Yingst, Kimberly L. Biedermann, and Aimee M. Monhead
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Atmospheric Science ,education.field_of_study ,Ecology ,Lithology ,Population ,Paleontology ,Soil Science ,Mineralogy ,Forestry ,Mars Exploration Program ,Aquatic Science ,Oceanography ,Roundness (geology) ,Sphericity ,Geophysics ,Impact crater ,Space and Planetary Science ,Geochemistry and Petrology ,Earth and Planetary Sciences (miscellaneous) ,Sedimentary rock ,education ,Pebble ,Geology ,Earth-Surface Processes ,Water Science and Technology - Abstract
[1] We adapt and test a standard terrestrial technique of assessing morphology quantitatively for use with sites on Mars based on two-dimensional equations and particle outlines, whereby images of particles obtained remotely may yield dimensionless, numerical shape and roundness values consistent with previous knowledge of the lithology and sedimentary transport history. Our test site was the particle-rich Rock Garden at the Mars Pathfinder landing site, a location where the primary geologic processes and lithology have been determined by other means. A total of 575 particles were assessed in terms of size, sphericity, elongation, and roundness; qualitative roundness was determined for 460 particles. Particles are mostly pebble- to cobble-sized and have an average sphericity of 0.75, elongation of 0.63, and relative roundness of 0.083; 69% of particles are subangular or subrounded. Particle sphericity is unimodal, with a size-sphericity profile matching trends for terrestrial populations of similar lithology and elongations nearly identical to those for particles at Vikings 1 and 2. This matches the predictions for a site with the single overall lithology implied from other analyses. Roundness data indicate one or possibly two particle populations, representing the primary processes that likely affected particle roundness most strongly: impact and catastrophic flooding. Finally, we tested a hypothesis suggesting that darker, smaller, more angular particles comprise a population transported through impact cratering, while larger, less dark, more rounded particles are associated with catastrophic flood transport. The opposite result is seen: larger particles throughout the Rock Garden are more angular than smaller ones.
- Published
- 2007
105. Wisconsin's Student Satellite Initiative: Launching Student Experiments into a Near-Space Environment
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R. Aileen Yingst, William Farrow, Elijah Tracking Payload Team, and Wet Behind the Ears Engineers
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Engineering ,ComputingMilieux_THECOMPUTINGPROFESSION ,Higher education ,Task force ,business.industry ,Library science ,Space (commercial competition) ,Near space ,Engineering management ,Work (electrical) ,Workforce ,ComputingMilieux_COMPUTERSANDEDUCATION ,Satellite ,business ,Aerospace - Abstract
In Wisconsin, promising science and engineering students who are interested in pursuing various aerospace fields often believe that they must look outside the state to gain the education and experience they need to excel in fields of study that would serve to strengthen the workforce pool from which aerospace fields may draw. The Wisconsin Space Grant Consortium has supported several facets of a rapidly growing initiative, the WSGC Student Satellite Program. This initiative, headed by a task force made up of individuals representing industry, not-for-profits and higher education, brings together the crucial stakeholders in Wisconsin aerospace to work towards the common goal of recruiting and training the best and brightest students for careers in aerospace. The initiative has two prongs: a high-altitude balloon project, and a student-designed rocket project, both designed to carry student-designed and –built payloads.
- Published
- 2004
106. Sands at Gusev Crater, Mars
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Cabrol, Nathalie A., primary, Herkenhoff, Kenneth, additional, Knoll, Andrew H., additional, Farmer, Jack, additional, Arvidson, Raymond, additional, Grin, Edmond, additional, Li, Ronxing, additional, Fenton, Lori, additional, Cohen, Barbara, additional, Bell, James F., additional, and Aileen Yingst, R., additional
- Published
- 2014
- Full Text
- View/download PDF
107. Spectral evidence of volcanic cryptodomes on the northern plains of Mars
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Farrand, William H., primary, Lane, Melissa D., additional, Edwards, Benjamin R., additional, and Aileen Yingst, R., additional
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- 2011
- Full Text
- View/download PDF
108. MAHLI on Mars: lessons learned operating a geoscience camera on a landed payload robotic arm.
- Author
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Aileen Yingst, R., Edgett, Kenneth S., Kennedy, Megan R., Krezoski, Gillian M., McBride2,a, Marie J., Minitti, Michelle E., Ravine, Michael A., and Williams, Rebecca M. E.
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EARTH sciences , *MARTIAN surface , *MARS (Planet) , *LANDSCAPE assessment , *GEOLOGY , *GEOMORPHOLOGY - Abstract
The Mars Hand Lens Imager (MAHLI) is a 2-megapixel, color camera with resolution as high as 13.9 µm pixel−1 . MAHLI has operated successfully on the Martian surface for over 1150 Martian days (sols) aboard the Mars Science Laboratory (MSL) rover, Curiosity. During that time MAHLI acquired images to support science and science-enabling activities, including rock and outcrop textural analysis; sand characterization to further the understanding of global sand properties and processes; support of other instrument observations; sample extraction site documentation; range-finding for arm and instrument placement; rover hardware and instrument monitoring and safety; terrain assessment; landscape geomorphology; and support of rover robotic arm commissioning. Operation of the instrument has demonstrated that imaging fully illuminated, dust-free targets yields the best results, with complementary information obtained from shadowed images. The light-emitting diodes (LEDs) allow satisfactory night imaging but do not improve daytime shadowed imaging. MAHLI’s combination of finescale, science-driven resolution, RGB color, the ability to focus over a large range of distances, and relatively large field of view (FOV), have maximized the return of science and science-enabling observations given the MSL mission architecture and constraints. [ABSTRACT FROM AUTHOR]
- Published
- 2015
- Full Text
- View/download PDF
109. UPDATE ON CREATING CRATER CATALOGS OF THE APOLLO 15-16-17 LANDING SITES.
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Jodhpurkar, Mohini J., Ostrach, Lillian R., Brent Garry, W., Mest, Scott C., Aileen Yingst, R., Petro, Noah E., and Cohen, Barbara A.
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GEOLOGICAL mapping ,GEOLOGICAL maps ,CATALOGS ,CATALOGING ,LUNAR craters - Abstract
The pre-mission Apollo 15, 16, and 17 geologic maps have not been updated in approximately forty years, and the availability of recently acquired high-resolution images, multispectral data, and detailed topography and gravity data, when coupled with the Apollo field observations and decades of sample analyses, makes this a prime opportunity to do so. These areas were selected because they are more geologically diverse, the missions covered greater traverse distances, and there were additional science investigations associated with them. This investigation will produce 6 new USGS Special Investigation Maps at the regional (1:200,000) and landing site (1:24,000) scales to take advantage of the higher resolution of the Lunar Reconnaissance Orbiter Wide Angle Camera and Narrow Angle Camera base maps. Concurrent with the mapping efforts led by the project team, we collected measurements of craters ≥500 m on the 1:200,000 maps and ≥10 m on the 1:24,000 maps for all six map areas using the CraterTools extension, excluding secondaries and the areas containing them. To date, we have mapped ~640 and ~8250 craters for the Apollo 15 regional and landing site maps respectively, ~900 and ~6480 craters for the Apollo 16 maps, and ~830 and ~4110 for the Apollo 17 maps. Once the geologic units on each map are finalized, we can make more detailed age interpretations based on these crater catalogs. [ABSTRACT FROM AUTHOR]
- Published
- 2020
110. UPDATING THE GEOLOGIC MAPS OF THE APOLLO 15-16-17 LANDING SITES – YEAR 2.
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Brent Garry, W., Aileen Yingst, R., Mest, Scott C., Ostrach, Lillian R., and Jodhpurkar, Mohini J.
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GEOLOGICAL mapping ,SENSE data ,REMOTE sensing ,DATA mapping - Abstract
Our team is funded by NASA PDART to produce updated geologic maps of the Apollo 15-16-17 landing sites at regional (1:200,000) and landing site (1:24,000) map scales for publication in the USGS SIM series. Our new maps will incorporate findings and interpretations from nearly 50 years of studies of the original Apollo data, surface observations, and sample analyses, as well as recent remote sensing data. Task 1. Renovation of Pre-Mission Geologic Maps: We have renovated the regional (1:250,000) and landing site (1:50,000) maps for Apollo 15, 16, and 17 pre-mission geologic maps in ArcMap and are in the process of finalizing the GIS file submission to the USGS for archiving. Task 2. Updating the Geologic Map of Apollo 15-16-17 Landing Sites: Mapping of the updated geologic maps continues in year 2 with the focus on defining point features and structural/linear features. We have also included Kaguya Terrain Camera mosaics as supporting data for mapping regional features. Task 3. Determine crater derived ages for new units: Craters ≥500 m have been mapped on the regional (1:200,000) Lunar Reconnaissance Orbiter Wide Angle Camera basemaps and craters ≥10 m have been mapped on the Narrow Angle Camera (NAC) basemaps for each landing site (1:24,000). Once map units are defined, these counts will be used to interpret unit ages on each map. [ABSTRACT FROM AUTHOR]
- Published
- 2020
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