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    <title>Earth Science Picture of the Day</title>
    
    <link rel="alternate" type="text/html" href="http://epod.usra.edu/blog/" />
    <id>tag:typepad.com,2003:weblog-1820629</id>
    <updated>2012-01-27T03:01:00-05:00</updated>
    <subtitle>Each day a different image or photograph is featured, with an 
accompanying caption, which deals with various topics in Earth Science.
</subtitle>
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        <title>Milky Way Viewed from Reunion Island</title>
        <link rel="alternate" type="text/html" href="http://epod.usra.edu/blog/2012/01/milky-way-viewed-from-reunion-island.html" />
        <link rel="replies" type="text/html" href="http://epod.usra.edu/blog/2012/01/milky-way-viewed-from-reunion-island.html" />
        <id>tag:typepad.com,2003:post-6a0105371bb32c970b0162ff91399b970d</id>
        <published>2012-01-27T03:01:00-05:00</published>
<updated>2012-01-27T03:01:00-05:00</updated>
                <summary>Photographer: Luc Perrot; Luc's Web site Summary Author: Luc Perrot; Jim Foster This photo above shows the Milky Way as observed from Reunion Island in the Indian Ocean on the night of November 3, 2011. In the lower part of...</summary>
                        <content type="html" xml:lang="en-US" xml:base="http://epod.usra.edu/blog/">&lt;div xmlns="http://www.w3.org/1999/xhtml"&gt;&lt;p&gt;&lt;a href="http://epod.usra.edu/.a/6a0105371bb32c970b01676086eadc970b-pi" style="display: inline;"&gt;&lt;img alt="Reunion-Island_luc-perrot" class="asset  asset-image at-xid-6a0105371bb32c970b01676086eadc970b" src="http://epod.usra.edu/.a/6a0105371bb32c970b01676086eadc970b-750wi" style="width: 720px;" title="Reunion-Island_luc-perrot"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br&gt;&lt;strong&gt;&lt;br&gt;Photographer&lt;/strong&gt;: &lt;a href="mailto:luc.perrot@wanadoo.fr" target="_self"&gt;Luc Perrot&lt;/a&gt;; &lt;a href="http://www.lucperrot.fr/" target="_self"&gt;Luc's Web site&lt;/a&gt;  &lt;br&gt;&lt;strong&gt;Summary Author&lt;/strong&gt;: &lt;a href="mailto:luc.perrot@wanadoo.fr" target="_self"&gt;Luc Perrot&lt;/a&gt;; &lt;a href="mailto:james.l.foster@nasa.gov" target="_self"&gt;Jim Foster&lt;br&gt;&lt;/a&gt;&lt;br&gt;This photo above shows the &lt;span style="color: #0000ff;"&gt;&lt;a href="http://messier.seds.org/more/mw.html" target="_self"&gt;Milky Way&lt;/a&gt;&lt;/span&gt; as observed from &lt;span style="color: #0000ff;"&gt;&lt;a href="http://en.wikipedia.org/wiki/R%C3%A9union" target="_self"&gt;Reunion Island&lt;/a&gt;&lt;/span&gt; in the Indian Ocean on the night of November 3, 2011. In the lower part of the picture, between two old &lt;span style="color: #0000ff;"&gt;&lt;a href="http://www.uni-graz.at/~katzer/engl/Tama_ind.html" target="_self"&gt;tamarind trees&lt;/a&gt;&lt;/span&gt;, my silhouette is illuminated by a headlamp I'm wearing as I gaze toward the constellation of &lt;span style="color: #0000ff;"&gt;&lt;a href="http://www.topastronomer.com/StarCharts/Constellations/Scorpius.php" target="_self"&gt;Scorpio&lt;/a&gt;&lt;/span&gt; and the &lt;span style="color: #0000ff;"&gt;&lt;a href="http://en.wikipedia.org/wiki/Galactic_Center" target="_self"&gt;galactic center&lt;/a&gt;&lt;/span&gt;. The stars that comprise Scorpio are wrapped around one of the the densest parts of &lt;a href="http://www.atlasoftheuniverse.com/galaxy.html" target="_self"&gt;our galaxy&lt;/a&gt;. Note that the brightest star in Scorpio, the &lt;a href="http://hyperphysics.phy-astr.gsu.edu/hbase/astro/redsup.html" target="_self"&gt;red supergiant&lt;/a&gt;, &lt;a href="http://stars.astro.illinois.edu/sow/antares.html" target="_self"&gt;Antares&lt;/a&gt;, is at upper left -- the tail of the scorpion curls about the tamarind at right. This is how the night sky appears in a truly &lt;span style="color: #0000ff;"&gt;&lt;a href="http://www.darksky.org/" target="_self"&gt;dark location&lt;/a&gt;&lt;/span&gt; -- becoming increasingly more difficult to find.&lt;/p&gt;&#xD;
&lt;ul class="related-clicks"&gt;&#xD;
&lt;li class="coords"&gt;Plaine des Cafres, Réunion Island Coordinates: &lt;a href="http://www.panoramio.com/map/#lt=-21.114444&amp;amp;ln=55.532500&amp;amp;z=5&amp;amp;k=2&amp;amp;a=1&amp;amp;tab=2&amp;amp;pl=all" target="_self"&gt;-21.114444, 55.5325&lt;/a&gt; &lt;/li&gt;&#xD;
&lt;li class="related"&gt;Related Links             &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2011/05/milky-way-from-northern-ireland.html" target="_self"&gt;Milky Way from Northern Ireland&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="Reunion Island Basalt" target="_self"&gt;Reunion Island Basalt&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://www.nasa.gov/multimedia/imagegallery/image_feature_784.html" target="_self"&gt;Light Echoes From a Red Supergiant&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://www.odec.ca/projects/2002/wongj/public_html/Index.htm" target="_self"&gt;The Formation, Evolution and Death of Stars&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://rsd-www.nrl.navy.mil/7213/lazio/GC/" target="_self"&gt;The Galactic Center: A Wide-Field, Low-Frequency Image&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;li class="eo"&gt;Earth Observatory             &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/blogs/elegantfigures/2010/09/21/odds-ends-the-milky-way/" target="_self"&gt;The Milky Way&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/NaturalHazards/view.php?id=9176" target="_self"&gt;Reunion Island Volcano Erupts&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;/ul&gt;&lt;/div&gt;
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    </entry>
    <entry>
        <title>Mount Baker in Filtered Sunlight</title>
        <link rel="alternate" type="text/html" href="http://epod.usra.edu/blog/2012/01/mount-baker-in-filtered-sunlight.html" />
        <link rel="replies" type="text/html" href="http://epod.usra.edu/blog/2012/01/mount-baker-in-filtered-sunlight.html" />
        <id>tag:typepad.com,2003:post-6a0105371bb32c970b0168e5cd5f04970c</id>
        <published>2012-01-26T03:01:00-05:00</published>
<updated>2012-01-26T03:01:00-05:00</updated>
                <summary>Photographer: Robert Farrimond Summary Authors: Robert Farrimond Mount Baker, at 10,778 ft (3,285 m), is one of several large stratovolcanoes in Washington State. Part of the Pacific Ring of Fire, it's widely accepted that the volcanoes in this region are...</summary>
                        <content type="html" xml:lang="en-US" xml:base="http://epod.usra.edu/blog/">&lt;div xmlns="http://www.w3.org/1999/xhtml"&gt;&lt;p&gt;&lt;a href="http://epod.usra.edu/.a/6a0105371bb32c970b0168e5cd6931970c-pi" style="display: inline;"&gt;&lt;img alt="Baker2" class="asset  asset-image at-xid-6a0105371bb32c970b0168e5cd6931970c" src="http://epod.usra.edu/.a/6a0105371bb32c970b0168e5cd6931970c-750wi" style="width: 720px;" title="Baker2"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br&gt;&lt;br&gt;&lt;strong&gt;Photographer&lt;/strong&gt;: &lt;a href="mailto:beeowulf@netzero.com" target="_self"&gt;Robert Farrimond&lt;/a&gt; &lt;br&gt;&lt;strong&gt;Summary Authors&lt;/strong&gt;: &lt;a href="mailto:beeowulf@netzero.com" target="_self"&gt;Robert Farrimond&lt;/a&gt;&lt;br&gt;&lt;br&gt;Mount Baker, at 10,778 ft (3,285 m), is one of &lt;a href="http://nationalatlas.gov/dynamic/dyn_vol-wa.html" target="_self"&gt;several&lt;/a&gt; large &lt;a href="http://www.volcano.si.edu/education/tpgallery.cfm?category=Stratovolcanoes" target="_self"&gt;stratovolcanoes&lt;/a&gt; in &lt;a href="http://en.wikipedia.org/wiki/Washington_%28state%29" target="_self"&gt;Washington State&lt;/a&gt;. Part of the &lt;a href="http://pubs.usgs.gov/gip/dynamic/fire.html" target="_self"&gt;Pacific Ring of Fire&lt;/a&gt;, it's widely accepted that the volcanoes in this region are a result of &lt;a href="http://earthquake.usgs.gov/learn/glossary/?term=subduction" target="_self"&gt;subduction&lt;/a&gt; of the &lt;a href="http://vulcan.wr.usgs.gov/Volcanoes/JuanDeFucaRidge/description_juan_de_fuca.html" target="_self"&gt;Juan De Fuca&lt;/a&gt; &lt;a href="http://pubs.usgs.gov/gip/dynamic/tectonic.html" target="_self"&gt;tectonic plate&lt;/a&gt; under the &lt;a href="http://www.classzone.com/books/earth_science/terc/content/investigations/es0810/es0810page08.cfm" target="_self"&gt;North American Plate&lt;/a&gt;. &lt;a href="http://vulcan.wr.usgs.gov/Glossary/StratoVolcano/description_composite_volcano.html" target="_self"&gt;Stratovolcanoes &lt;/a&gt;are known for extremely &lt;a href="http://www.uwec.edu/jolhm/EH3/Group1/Website/Stratovolcano.html" target="_self"&gt;violent eruptions&lt;/a&gt;, sometimes with far reaching effects. Mt. Baker’s last known notable &lt;a href="http://www.pep-c.org/mountbaker/" target="_self"&gt;eruption&lt;/a&gt; occurred more than 150 years ago. A field of corn ready for harvest is in the foreground. Photo taken October 8, 2011.&lt;br&gt;&lt;br&gt;&lt;strong&gt;Photo details: &lt;/strong&gt;Canon 1000D/XS; Shooting Mode: A-DEP; Tv (Shutter Speed): 1/4000; Av (Aperture Value): 9.5; Metering Mode: Evaluative Metering; Exposure Compensation: -2; ISO Speed: 800; Lens: EF28-105mm f/3.5-4.5 USM; Focal Length: 105.0mm; Image Quality: RAW.&lt;/p&gt;&#xD;
&lt;ul class="related-clicks"&gt;&#xD;
&lt;li class="coords"&gt;Mount Baker Coordinates: &lt;a href="http://www.panoramio.com/map/#lt=48.777343&amp;amp;ln=-121.813201&amp;amp;z=4&amp;amp;k=2&amp;amp;a=1&amp;amp;tab=1&amp;amp;pl=all" target="_self"&gt;48.777343, -121.813201&lt;/a&gt; &lt;/li&gt;&#xD;
&lt;li class="related"&gt;Related Links                &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2003/10/mount-baker-and-cloud.html" target="_self"&gt;Mount Baker and Cloud&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://mbvo.wwu.edu/index.shtml" target="_self"&gt;Mount Baker Volcano Research Center &lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/Mount_Baker_from_Above_IMAG0564.jpg" target="_self"&gt;Stu Witmer's Photo of Mount Baker from Above&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://geomaps.wr.usgs.gov/pacnw/nc/baker1.html" target="_self"&gt;Geologic Map of Mount Baker&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://www.platetectonics.com/book/page_2.asp" target="_self"&gt;About Plate Tectonics&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://www.ngdc.noaa.gov/hazard/stratoguide/stratoguide.pdf" target="_self"&gt;A Teacher's Guide to Stratovolcanoes&lt;/a&gt; [pdf]&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;li class="eo"&gt;Earth Observatory                &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/IOTD/view.php?id=4569" target="_self"&gt;Mount Baker, Washington—a Hazardous Beauty&lt;/a&gt;&lt;strong&gt;&lt;/strong&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;/ul&gt;&lt;/div&gt;
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    </entry>
    <entry>
        <title>Travertine</title>
        <link rel="alternate" type="text/html" href="http://epod.usra.edu/blog/2012/01/travertine.html" />
        <link rel="replies" type="text/html" href="http://epod.usra.edu/blog/2012/01/travertine.html" />
        <id>tag:typepad.com,2003:post-6a0105371bb32c970b0162ffccc464970d</id>
        <published>2012-01-25T03:01:00-05:00</published>
<updated>2012-01-25T03:01:00-05:00</updated>
                <summary>Photographer: Wendy Van Norden Summary Author: Wendy Van Norden The photo above shows travertine covering the outside surface of the J. Paul Getty Museum in Los Angeles, California. In this close-up, you can clearly see leaf fossils, evidence of the...</summary>
                        <content type="html" xml:lang="en-US" xml:base="http://epod.usra.edu/blog/">&lt;div xmlns="http://www.w3.org/1999/xhtml"&gt;&lt;p&gt;&lt;a href="http://epod.usra.edu/.a/6a0105371bb32c970b016760c139e6970b-pi" style="display: inline;"&gt;&lt;img alt="Travertinephoto (9)" class="asset  asset-image at-xid-6a0105371bb32c970b016760c139e6970b" src="http://epod.usra.edu/.a/6a0105371bb32c970b016760c139e6970b-750wi" style="width: 720px;" title="Travertinephoto (9)"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&#xD;
&lt;p&gt;&lt;strong&gt;Photographer&lt;/strong&gt;: &lt;a href="mailto:wvannorden@hw.com" target="_self"&gt;Wendy Van Norden&lt;/a&gt; &lt;br&gt;&lt;strong&gt;Summary Author&lt;/strong&gt;: &lt;a href="mailto:wvannorden@hw.com" target="_self"&gt;Wendy Van Norden&lt;/a&gt; &lt;br&gt;&lt;br&gt;The photo above shows &lt;a href="http://georneys.blogspot.com/2011/04/geology-word-of-week-t-is-for.html" target="_self"&gt;travertine&lt;/a&gt; covering the outside surface of the &lt;a href="http://www.getty.edu/museum/" target="_self"&gt;J. Paul Getty Museum&lt;/a&gt; in &lt;a href="http://en.wikipedia.org/wiki/Los_Angeles" target="_self"&gt;Los Angeles, California&lt;/a&gt;. In this close-up, you can clearly see leaf fossils, evidence of the shallow water environment in which the travertine formed. Rainwater becomes acidic when it absorbs &lt;a href="http://www.eoearth.org/article/Carbon_dioxide" target="_self"&gt;carbon dioxide&lt;/a&gt; (CO2) from the air. As this rainwater seeps into the ground, it dissolves the &lt;a href="http://geology.com/minerals/calcite.shtml" target="_self"&gt;calcite&lt;/a&gt; in &lt;a href="http://www.galleries.com/rocks/limestone.htm" target="_self"&gt;limestone&lt;/a&gt; layers. If this water should make its way back to the surface, bubbling up from a spring, for example, the saturated &lt;a href="http://www.groundwater.org/kc/whatis.html" target="_self"&gt;groundwater&lt;/a&gt; would release the CO2 and precipitate the calcite around &lt;a href="http://en.wikipedia.org/wiki/Algae" target="_self"&gt;algal&lt;/a&gt; mats, &lt;a href="http://www.ucmp.berkeley.edu/bacteria/bacteria.html" target="_self"&gt;bacteria&lt;/a&gt; and even leaves. &lt;br&gt;&lt;br&gt;The travertine of the &lt;a href="http://www.getty.edu/news/press/arch/archdesc.html" target="_self"&gt;Getty Museum&lt;/a&gt; comes from the most famous travertine quarry in the world, the &lt;a href="http://www.mmdtkw.org/VTravertine.html" target="_self"&gt;Bagni di Tivoli&lt;/a&gt;, which is located east of &lt;a href="http://en.wikipedia.org/wiki/Rome" target="_self"&gt;Rome, Italy&lt;/a&gt;. It's the same travertine used to build the &lt;a href="http://www.aviewoncities.com/rome/colosseo.htm" target="_self"&gt;Coliseum&lt;/a&gt;, the &lt;a href="http://www.aviewoncities.com/rome/trevi.htm" target="_self"&gt;Trevi Fountain&lt;/a&gt; and the colonnade of &lt;a href="http://www.vaticanstate.va/EN/Monuments/Saint_Peters_Basilica/" target="_self"&gt;Saint Peter's Basilica&lt;/a&gt;. This rock started forming approximately 80,000 years ago -- the quarry has been active for about the last 2,000 years. Typically, travertine is cut across the &lt;a href="http://sepmstrata.org/terminology/beddingplane.html" target="_self"&gt;bedding planes&lt;/a&gt;, revealing the layering of the rock. Travertine is lighter than &lt;a href="http://geology.com/rocks/granite.shtml" target="_self"&gt;granite&lt;/a&gt;, easier to cut, and capable of carrying heavy loads. &lt;a href="http://architect.architecture.sk/richard-meier-architect/richard-meier-architect.php" target="_self"&gt;Richard Meier&lt;/a&gt;, the architect for the Getty Museum, didn’t need the rock to bear great weights. He chose instead to highlight the wonderful texture of the rock, so he had the rock cut parallel to the bedding planes.  As a result, when visiting the Getty Museum, one is able to admire the intricate texture and abundant fossils preserved in an ancient Roman spring. Photo taken on November 13, 2011.&lt;/p&gt;&#xD;
&lt;p&gt;&lt;strong&gt;Photo details&lt;/strong&gt;: Camera Maker: Apple; Camera Model: iPhone 4S; Focal Length: 4.3mm (35mm equivalent: 35mm); Aperture: f/2.4; Exposure Time: 0.0018 s (1/557); ISO equiv: 64; Metering Mode: Matrix; Exposure: program (Auto); White Balance: Auto; Flash Fired: No (enforced); Orientation: Rotate 90; Color Space: sRGB; Software: 5.0.1.&lt;/p&gt;&#xD;
&lt;ul class="related-clicks"&gt;&#xD;
&lt;li class="coords"&gt;J. Paul Getty Museum, Los Angeles Coordinates: &lt;a href="http://www.panoramio.com/map/#lt=34.077167&amp;amp;ln=-118.475000&amp;amp;z=0&amp;amp;k=2&amp;amp;a=1&amp;amp;tab=1&amp;amp;pl=all" target="_self"&gt;34.077167, -118.475000&lt;/a&gt; &lt;/li&gt;&#xD;
&lt;li class="related"&gt;Related Links          &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2007/08/reddish-sky-reflected-on-travertine-terraces.html" target="_self"&gt;Reddish Sky Reflected on Travertine Terraces&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2004/03/orange-mound-spring.html" target="_self"&gt;Orange Mound Spring&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://www.algaebase.org/" target="_self"&gt;Algaebase&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;li class="eo"&gt;Earth Observatory          &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/IOTD/view.php?id=2343" target="_self"&gt;Los Angeles&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/IOTD/view.php?id=3545" target="_self"&gt;Rome&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;/ul&gt;&lt;/div&gt;
&lt;p&gt;&lt;a href="http://feedads.g.doubleclick.net/~a/zNt2GZ_3muxIgezMvEAth2vzMnM/0/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/zNt2GZ_3muxIgezMvEAth2vzMnM/0/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br/&gt;
&lt;a href="http://feedads.g.doubleclick.net/~a/zNt2GZ_3muxIgezMvEAth2vzMnM/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/zNt2GZ_3muxIgezMvEAth2vzMnM/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/EarthSciencePictureOfTheDay/~4/QFTQLqOeZsQ" height="1" width="1"/&gt;</content>


    </entry>
    <entry>
        <title>Breccia in Death Valley</title>
        <link rel="alternate" type="text/html" href="http://epod.usra.edu/blog/2012/01/breccia-in-death-valley.html" />
        <link rel="replies" type="text/html" href="http://epod.usra.edu/blog/2012/01/breccia-in-death-valley.html" />
        <id>tag:typepad.com,2003:post-6a0105371bb32c970b0162ffbd56b9970d</id>
        <published>2012-01-24T03:01:00-05:00</published>
<updated>2012-01-24T03:01:00-05:00</updated>
                <summary>Photographer: Rick Scott; Rick's Web site Summary Author: Rick Scott; Jim Foster The photo above showing a huge outcrop of breccia was taken in Fall Canyon at Death Valley National Park, California. Breccia typically forms when angular fragments (over 2mm...</summary>
                        <content type="html" xml:lang="en-US" xml:base="http://epod.usra.edu/blog/">&lt;div xmlns="http://www.w3.org/1999/xhtml"&gt;&lt;p&gt;&lt;a href="http://epod.usra.edu/.a/6a0105371bb32c970b0168e5b3231a970c-pi" style="display: inline;"&gt;&lt;img alt="Breccia_in_Fall_Canyon_Death_Valley_Rick_Scott (2)" class="asset  asset-image at-xid-6a0105371bb32c970b0168e5b3231a970c" src="http://epod.usra.edu/.a/6a0105371bb32c970b0168e5b3231a970c-750wi" style="width: 720px;" title="Breccia_in_Fall_Canyon_Death_Valley_Rick_Scott (2)"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br&gt;&lt;br&gt;&lt;strong&gt;Photographer&lt;/strong&gt;: &lt;a href="mailto:rmscott@cox.net" target="_self"&gt;Rick Scott&lt;/a&gt;; Rick's &lt;a href="http://naturalimagesgallery.com" target="_self"&gt;Web site&lt;/a&gt; &lt;br&gt;&lt;strong&gt;Summary Author&lt;/strong&gt;:&lt;a href="mailto:rmscott@cox.net" target="_self"&gt; Rick Scott&lt;/a&gt;; &lt;a href="mailto:james.l.foster@nasa.gov" target="_self"&gt;Jim Foster&lt;/a&gt;&lt;br&gt;&lt;br&gt;The photo above showing a huge outcrop of &lt;a href="http://geology.com/rocks/breccia.shtml" target="_self"&gt;breccia&lt;/a&gt; was taken in &lt;a href="http://www.americansouthwest.net/slot_canyons/death_valley/fall_canyon.html" target="_self"&gt;Fall Canyon&lt;/a&gt; at &lt;a href="http://www.nps.gov/deva/index.htm" target="_self"&gt;Death Valley National Park&lt;/a&gt;, California. Breccia typically forms when angular fragments (over 2mm in diameter) of rock accumulate in streambeds and &lt;a href="http://geomaps.wr.usgs.gov/parks/deva/rfan.html" target="_self"&gt;alluvial fans&lt;/a&gt;, for instance. The pieces become bound by mineral &lt;a href="http://www.geolsoc.org.uk/gsl/pid/3559;jsessionid=04EAE81C4F5D1813684981062D4C978C" target="_self"&gt;cement&lt;/a&gt; or are fixed by much smaller particles that fill the spaces between the angular pieces. A &lt;a href="http://earthsci.org/flooding/unit3/u3-03-04.html" target="_self"&gt;debris flow&lt;/a&gt; is one condition where binding of the fragments can happen. Another such condition is a meteor &lt;a href="http://www.lpi.usra.edu/education/explore/shaping_the_planets/impact_cratering.shtml" target="_self"&gt;impact crater&lt;/a&gt;. Breccia is similar to &lt;a href="http://flexiblelearning.auckland.ac.nz/rocks_minerals/rocks/conglomerate.html" target="_self"&gt;conglomerate&lt;/a&gt;, but in conglomerate the fragments are more rounded, indicating that they've traveled further (are more eroded) before cementation occurs. Photo taken on November 26, 2011. &lt;br&gt;&lt;br&gt;&lt;strong&gt;Photo details&lt;/strong&gt;: Camera Maker: Canon; Camera Model: Canon EOS 40D; Lens: EF16-35mm f/2.8L USM; Focal Length: 35mm; Focus Distance: Infinite; Aperture: f/8.0; Exposure Time: 0.033 s (1/30); ISO equiv: 100; Exposure Bias: none; Metering Mode: Matrix; Exposure Mode: Manual; White Balance: Manual; Flash Fired: No (enforced); Orientation: Normal; Color Space: sRGB ; RAW Mode; Software: Adobe Photoshop CS5 Windows.&lt;/p&gt;&#xD;
&lt;ul class="related-clicks"&gt;&#xD;
&lt;li class="coords"&gt;Coordinates: &lt;a href="http://www.panoramio.com/map/#lt=36.83105&amp;amp;ln=-117.17451&amp;amp;z=3&amp;amp;k=2" target="_self"&gt;36.83105, -117.17451&lt;/a&gt; &lt;/li&gt;&#xD;
&lt;li class="related"&gt;Related Links            &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2007/01/breccia-outcrop-in-manicouagan-impact-structure.html" target="_self"&gt;Breccia Outcrop in Manicouagan Impact Structure&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://vulcan.wr.usgs.gov/Glossary/Lahars/description_lahars.html" target="_self"&gt;USGS: Debris Flows, Mudflows, Jökulhlaups, and Lahars&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://geology.com/meteor-impact-craters.shtml" target="_self"&gt;Meteor Craters - Asteroid Impact Sites&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://www.solarviews.com/eng/tercrate.htm" target="_self"&gt;Terrestrial Impact Craters&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;li class="eo"&gt;Earth Observatory            &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/IOTD/view.php?id=6470" target="_self"&gt;Death Valley National Park&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;/ul&gt;&lt;/div&gt;
&lt;p&gt;&lt;a href="http://feedads.g.doubleclick.net/~a/CRyrZJK5SW-JyzmG-3hF7CQMyXU/0/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/CRyrZJK5SW-JyzmG-3hF7CQMyXU/0/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br/&gt;
&lt;a href="http://feedads.g.doubleclick.net/~a/CRyrZJK5SW-JyzmG-3hF7CQMyXU/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/CRyrZJK5SW-JyzmG-3hF7CQMyXU/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/EarthSciencePictureOfTheDay/~4/-aw3qZNZz4A" height="1" width="1"/&gt;</content>


    </entry>
    <entry>
        <title>Sirius Twinkling</title>
        <link rel="alternate" type="text/html" href="http://epod.usra.edu/blog/2012/01/sirius-twinkling.html" />
        <link rel="replies" type="text/html" href="http://epod.usra.edu/blog/2012/01/sirius-twinkling.html" />
        <id>tag:typepad.com,2003:post-6a0105371bb32c970b0168e5bd3f66970c</id>
        <published>2012-01-23T03:01:00-05:00</published>
<updated>2012-01-23T03:01:00-05:00</updated>
                <summary>Photographer: David Lynch Summary Author: David Lynch Twinkling is the rapid fluctuation in brightness and color of a star. It’s caused by slight changes in density of air pockets called “seeing cells” that move across the observer’s line of sight....</summary>
                        <content type="html" xml:lang="en-US" xml:base="http://epod.usra.edu/blog/">&lt;div xmlns="http://www.w3.org/1999/xhtml"&gt;&lt;p&gt;&lt;a href="http://epod.usra.edu/.a/6a0105371bb32c970b0168e5bf0ad1970c-pi" style="display: inline;"&gt;&lt;img alt="Sirius_twinkling_untitled" class="asset  asset-image at-xid-6a0105371bb32c970b0168e5bf0ad1970c" src="http://epod.usra.edu/.a/6a0105371bb32c970b0168e5bf0ad1970c-750wi" style="width: 720px;" title="Sirius_twinkling_untitled"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&#xD;
&lt;p&gt;&lt;strong&gt;Photographer&lt;/strong&gt;: &lt;a href="mailto:thule@earthlink.net" target="_self"&gt;David Lynch&lt;/a&gt; &lt;br&gt;&lt;strong&gt;Summary Author&lt;/strong&gt;: &lt;a href="mailto:thule@earthlink.net" target="_self"&gt;David Lynch&lt;/a&gt; &lt;br&gt;&lt;br&gt;&lt;a href="http://imagine.gsfc.nasa.gov/docs/ask_astro/answers/981217a.html" target="_self"&gt;Twinkling&lt;/a&gt; is the rapid fluctuation in brightness and color of a star. It’s caused by slight changes in &lt;a href="http://www.usatoday.com/weather/wdensity.htm" target="_self"&gt;density of air pockets&lt;/a&gt; called “seeing cells” that move across the observer’s line of sight. Air’s &lt;a href="http://hyperphysics.phy-astr.gsu.edu/hbase/geoopt/refr.html" target="_self"&gt;refractive index&lt;/a&gt; is determined, in part, by its density. Such undulations cause slight, momentary defocusing of the starlight resulting in brightness changes, also called &lt;a href="http://www.astrophys-assist.com/educate/starry/starrynight.htm" target="_self"&gt;scintillation&lt;/a&gt;. In extreme cases, the star’s position hops around. Twinkling also produces rapid color changes because air is slightly dispersive, i.e. the index of refraction varies slightly with &lt;a href="http://science-edu.larc.nasa.gov/EDDOCS/Wavelengths_for_Colors.html" target="_self"&gt;wavelength&lt;/a&gt;.&lt;br&gt; &lt;br&gt;Both brightness and color twinkling are shown here in a five-second exposure of &lt;a href="http://earthsky.org/brightest-stars/sirius-the-brightest-sta" target="_self"&gt;Sirius&lt;/a&gt; using a &lt;a href="http://en.wikipedia.org/wiki/Telephoto_lens" target="_self"&gt;telephoto lens&lt;/a&gt; that was wiggled slightly during the exposure. As the star‘s twinkling image skated around the &lt;a href="http://scienceworld.wolfram.com/physics/FocalPlane.html" target="_self"&gt;focal plane&lt;/a&gt;, it traced out graceful, colorful arcs, fading in some places, brightening in others.&lt;br&gt;&lt;br&gt;Here scintillation and telescope jitter, the bane of astronomers everywhere, have been recast into a stunningly beautiful image. Image taken on January 4, 2012.&lt;/p&gt;&#xD;
&lt;ul class="related-clicks"&gt;&#xD;
&lt;li class="related"&gt;Related Links           &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2004/12/comet-machholz-and-geminid-meteor.html" target="_self"&gt;Comet Machholz and Geminid Meteor&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2011/01/-animation-of-venus-shadow.html" target="_self"&gt;Animation of Venus’ Shadow&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://www.ur.umich.edu/9394/Feb07_94/18.htm" target="_self"&gt;Mystery of twinkling stars explained&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://www.grc.nasa.gov/WWW/k-12/airplane/airprop.html" target="_self"&gt;Air Properties Definitions&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://www.cloudynights.com/item.php?item_id=555" target="_self"&gt;Astronomical Seeing&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;li class="eo"&gt;Earth Observatory           &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/blogs/earthmatters/2011/09/28/where-are-the-stars/?src=eorss-blogs" target="_self"&gt;Where are the Stars?&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;/ul&gt;&lt;/div&gt;
&lt;p&gt;&lt;a href="http://feedads.g.doubleclick.net/~a/EuLAfxqv-txUmSTcfYwzutqmz1Y/0/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/EuLAfxqv-txUmSTcfYwzutqmz1Y/0/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br/&gt;
&lt;a href="http://feedads.g.doubleclick.net/~a/EuLAfxqv-txUmSTcfYwzutqmz1Y/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/EuLAfxqv-txUmSTcfYwzutqmz1Y/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/EarthSciencePictureOfTheDay/~4/hIfpyqp1anI" height="1" width="1"/&gt;</content>


    </entry>
    <entry>
        <title>Rocks to Roots</title>
        <link rel="alternate" type="text/html" href="http://epod.usra.edu/blog/2012/01/rocks-to-roots.html" />
        <link rel="replies" type="text/html" href="http://epod.usra.edu/blog/2012/01/rocks-to-roots.html" />
        <id>tag:typepad.com,2003:post-6a0105371bb32c970b0162ff719b8a970d</id>
        <published>2012-01-22T03:01:00-05:00</published>
<updated>2012-01-22T03:01:00-05:00</updated>
                <summary>Photographer: Dale Hugo Summary Author: Dale Hugo; Jim Foster As shown above, in Tettegouche State Park on the North Shore of Lake Superior, Minnesota, a family of northern white cedars (Thuja occidentalis) is ganging up on a hapless granite boulder....</summary>
                        <content type="html" xml:lang="en-US" xml:base="http://epod.usra.edu/blog/">&lt;div xmlns="http://www.w3.org/1999/xhtml"&gt;&lt;p&gt;&lt;a href="http://epod.usra.edu/.a/6a0105371bb32c970b01676068afd7970b-pi" style="display: inline;"&gt;&lt;img alt="Rocks to Roots" class="asset  asset-image at-xid-6a0105371bb32c970b01676068afd7970b" src="http://epod.usra.edu/.a/6a0105371bb32c970b01676068afd7970b-750wi" style="width: 720px;" title="Rocks to Roots"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br&gt; &lt;br&gt;&lt;strong&gt;Photographer&lt;/strong&gt;: &lt;a href="mailto:d.hugo@comcast.net" target="_self"&gt;Dale Hugo&lt;/a&gt;  &lt;br&gt;&lt;strong&gt;Summary Author&lt;/strong&gt;: &lt;a href="mailto:d.hugo@comcast.net" target="_self"&gt;Dale Hugo&lt;/a&gt;; &lt;a href="mailto:james.l.foster@nasa.gov" target="_self"&gt;Jim Foster&lt;/a&gt;&lt;br&gt; &lt;br&gt;As shown above, in &lt;a href="http://www.dnr.state.mn.us/state_parks/tettegouche/index.html" target="_self"&gt;Tettegouche State Park&lt;/a&gt; on the &lt;a href="http://www.northshorevisitor.com/" target="_self"&gt;North Shore&lt;/a&gt; of &lt;a href="http://www.dnr.state.wi.us/org/caer/ce/eek/nature/habitat/lakesuperior.htm" target="_self"&gt;Lake Superior&lt;/a&gt;, &lt;a href="http://en.wikipedia.org/wiki/Minnesota" target="_self"&gt;Minnesota&lt;/a&gt;, a family of northern &lt;a href="http://www.rook.org/earl/bwca/nature/trees/thujaocc.html" target="_self"&gt;white cedars&lt;/a&gt; (&lt;em&gt;&lt;a href="http://www.na.fs.fed.us/pubs/silvics_manual/volume_1/thuja/occidentalis.htm" target="_self"&gt;Thuja occidentalis&lt;/a&gt;&lt;/em&gt;) is ganging up on a hapless &lt;a href="http://geology.com/rocks/granite.shtml" target="_self"&gt;granite&lt;/a&gt; boulder. These hardy trees need an extensive root system to handle the heavy snow loads and occasional strong winds that rake the northwestern Lake Superior area. In addition, they're often trampled by tourists during the summer months. Eventually, they and their progency will break down the boulders and rocky material, reducing it to consolidated soil more inviting to other types of trees. &lt;a href="http://www.geography4kids.com/files/land_weathering.html" target="_self"&gt;Weathering&lt;/a&gt; by &lt;a href="http://www.labspaces.net/98448/Root_fungi_turn_rock_into_soil" target="_self"&gt;root fungi&lt;/a&gt; plays a principal role in this slow but sure process. Frost &lt;a href="http://www.windows2universe.org/earth/geology/sed_weathering.html" target="_self"&gt;weathering &lt;/a&gt;is also important in regions where &lt;a href="http://www.geolsoc.org.uk/gsl/pid/3562;jsessionid=488CD658E9321A06AA2BE3682D9A9E38" target="_self"&gt;freeze-thaw cycles&lt;/a&gt; are commonplace.&lt;/p&gt;&#xD;
&lt;p&gt;&lt;strong&gt;Photo details&lt;/strong&gt;: Camera Maker: Samsung Techwin; Camera Model: &amp;lt;Samsung D70 / D75 / S730 / S750&amp;gt;; Focal Length: 17.4mm (35mm equivalent: 106mm); Aperture: f/4.9; Exposure Time: 0.0020 s (1/500); ISO equiv: 80; Exposure Bias: none; Metering Mode: Matrix; Exposure: program (Auto); White Balance: Auto; Flash Fired: No (enforced); Orientation: Normal; Color Space: sRGB.&lt;/p&gt;&#xD;
&lt;ul class="related-clicks"&gt;&#xD;
&lt;li class="coords"&gt;Tettegouche State Park, Minnesota Coordinates: &lt;a href="http://www.panoramio.com/map/#lt=47.33583&amp;amp;ln=-91.19944&amp;amp;z=3&amp;amp;k=2" target="_self"&gt;47.33583, -91.19944&lt;/a&gt; &lt;/li&gt;&#xD;
&lt;li class="related"&gt;Related Links                    &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2010/10/biological-weathering-and-tree-roots.html" target="_self"&gt;Biological Weathering and Tree Roots&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2005/12/city-roots.html" target="_self"&gt;City Roots&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://my.ilstu.edu/~jrcarter/ice/diurnal/" target="_self"&gt;Ice Formations with Daily (Diurnal) Freeze/Thaw Cycles&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://www.ncbi.nlm.nih.gov/pubmed/522148" target="_self"&gt;Frost-weathering on Mars&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;li class="eo"&gt;Earth Observatory                    &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/NaturalHazards/view.php?id=52130" target="_self"&gt;Pagami Creek Fire in Minnesota&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;/ul&gt;&lt;/div&gt;
&lt;p&gt;&lt;a href="http://feedads.g.doubleclick.net/~a/OHEEYwOctlk1wHyhG-AtD83q-pQ/0/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/OHEEYwOctlk1wHyhG-AtD83q-pQ/0/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br/&gt;
&lt;a href="http://feedads.g.doubleclick.net/~a/OHEEYwOctlk1wHyhG-AtD83q-pQ/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/OHEEYwOctlk1wHyhG-AtD83q-pQ/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/EarthSciencePictureOfTheDay/~4/ETrCNBZA_mM" height="1" width="1"/&gt;</content>


    </entry>
    <entry>
        <title>Sundog and Bright Tail Over Trento, Italy</title>
        <link rel="alternate" type="text/html" href="http://epod.usra.edu/blog/2012/01/sundog-and-bright-tail-over-trento-italy.html" />
        <link rel="replies" type="text/html" href="http://epod.usra.edu/blog/2012/01/sundog-and-bright-tail-over-trento-italy.html" />
        <id>tag:typepad.com,2003:post-6a0105371bb32c970b0162ff650a3e970d</id>
        <published>2012-01-21T03:01:00-05:00</published>
<updated>2012-01-21T03:01:00-05:00</updated>
                <summary>Photographer: Alessandro Zotta; Alessandro's Web page Summary Author: Alessandro Zotta; Jim Foster The photo above showing a colorful sundog heeling the horizon was taken in Trento, Italy on the afternoon of November 29, 2011. Sundogs, also known as parhelia or...</summary>
                        <content type="html" xml:lang="en-US" xml:base="http://epod.usra.edu/blog/">&lt;div xmlns="http://www.w3.org/1999/xhtml"&gt;&lt;p&gt;&lt;a href="http://epod.usra.edu/.a/6a0105371bb32c970b0162ff67085b970d-pi" style="display: inline;"&gt;&lt;img alt="Sundog and Bright Tail Over Trento, Italy" class="asset  asset-image at-xid-6a0105371bb32c970b0162ff67085b970d" src="http://epod.usra.edu/.a/6a0105371bb32c970b0162ff67085b970d-750wi" style="width: 720px;" title="Sundog and Bright Tail Over Trento, Italy"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br&gt;&lt;strong&gt;&lt;br&gt;Photographer&lt;/strong&gt;: &lt;a href="mailto:zotenfriend@gmail.com" target="_self"&gt;Alessandro Zotta&lt;/a&gt;; Alessandro's &lt;a href="http://www.facebook.com/AlessandroZottaPhotography" target="_self"&gt;Web page&lt;/a&gt;&lt;br&gt;&lt;strong&gt;Summary Author&lt;/strong&gt;: &lt;a href="mailto:zotenfriend@gmail.com" target="_self"&gt;Alessandro Zotta&lt;/a&gt;; &lt;a href="mailto:james.l.foster@nasa.gov" target="_self"&gt;Jim Foster&lt;/a&gt;&lt;br&gt;&lt;br&gt;The photo above showing a colorful &lt;a href="http://www.atoptics.co.uk/halo/parhelia.htm" target="_self"&gt;sundog&lt;/a&gt; heeling the horizon was taken in &lt;a href="http://en.wikipedia.org/wiki/Trento" target="_self"&gt;Trento, Italy&lt;/a&gt; on the afternoon of November 29, 2011. Sundogs, also known as parhelia or mock Suns, form when plate-shaped, hexagonal &lt;a href="http://www.atoptics.co.uk/halo/crystals.htm" target="_self"&gt;ice crystals&lt;/a&gt; in &lt;a href="http://eo.ucar.edu/webweather/cirrus.html" target="_self"&gt;cirrus clouds&lt;/a&gt; are aligned horizontally. When such an alignment occurs, sunlight passes through the alternate side faces of the crystals, being &lt;a href="http://hyperphysics.phy-astr.gsu.edu/hbase/geoopt/refr.html" target="_self"&gt;bent&lt;/a&gt; 22 degrees from its original path. The bright tail of this sundog is actually a portion of the &lt;a href="http://www.weatherscapes.com/album.php?cat=optics&amp;amp;subcat=parhelic_circle" target="_self"&gt;parhelic circle&lt;/a&gt;. Note that the Sun is behind the mountain face at right -- at the same altitude as the sundog.&lt;br&gt;&lt;br&gt;&lt;strong&gt;Photo details&lt;/strong&gt;: Nikon Camera, Model D3100; 32 mm focal length ; aperture of f/10.0; exposure time of 0.003125 s (1/320); ISO equiv: 400; exposure bias, none. Time of photo 3:44 p.m.&lt;/p&gt;&#xD;
&lt;ul class="related-clicks"&gt;&#xD;
&lt;li class="coords"&gt;Trento, Italy coordinates: &lt;a href="http://www.panoramio.com/map/#lt=46.056489&amp;amp;ln=10.988871&amp;amp;z=3&amp;amp;k=2" target="_self"&gt;46.056489, 10.988871&lt;/a&gt; &lt;/li&gt;&#xD;
&lt;li class="related"&gt;Related Links           &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2008/05/portland-maine-sundog-and-tail-from-aloft.html" target="_self"&gt;Portland, Maine Sundog and Tail from Aloft&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/Flowery_Branch-20111126-00084.jpg" target="_self"&gt;John Grainger’s Sundogs and Glint Photo &lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://science.nasa.gov/science-news/science-at-nasa/2002/24oct_sunrings/" target="_self"&gt;Rings Around the Sun&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;li class="eo"&gt;Earth Observatory           &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/IOTD/view.php?id=44124" target="_self"&gt;City lights at night along the France-Italy Border&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;/ul&gt;&lt;/div&gt;
&lt;p&gt;&lt;a href="http://feedads.g.doubleclick.net/~a/37xyPjjTFXiFZaX6GCunCn9gOOo/0/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/37xyPjjTFXiFZaX6GCunCn9gOOo/0/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br/&gt;
&lt;a href="http://feedads.g.doubleclick.net/~a/37xyPjjTFXiFZaX6GCunCn9gOOo/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/37xyPjjTFXiFZaX6GCunCn9gOOo/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/EarthSciencePictureOfTheDay/~4/mXe2Si61hno" height="1" width="1"/&gt;</content>


    </entry>
    <entry>
        <title>Was This on My Lens!?</title>
        <link rel="alternate" type="text/html" href="http://epod.usra.edu/blog/2012/01/was-this-on-my-lens.html" />
        <link rel="replies" type="text/html" href="http://epod.usra.edu/blog/2012/01/was-this-on-my-lens.html" />
        <id>tag:typepad.com,2003:post-6a0105371bb32c970b0167606b5e9d970b</id>
        <published>2012-01-20T03:01:00-05:00</published>
<updated>2012-01-20T03:01:00-05:00</updated>
                <summary>Photographer: Jens Hackmann Summary Author: Jens Hackmann; Jim Foster Have you ever looked at a picture you've taken and wondered "How in the world did THAT thing get on my lens?" In this case, the "thing" isn't a turbo-charged worm...</summary>
                        <content type="html" xml:lang="en-US" xml:base="http://epod.usra.edu/blog/">&lt;div xmlns="http://www.w3.org/1999/xhtml"&gt;&lt;p&gt;&lt;a href="http://epod.usra.edu/.a/6a0105371bb32c970b0162ff767a9a970d-pi" style="display: inline;"&gt;&lt;img alt="Jetcontrail by jensloeffel01" class="asset  asset-image at-xid-6a0105371bb32c970b0162ff767a9a970d" src="http://epod.usra.edu/.a/6a0105371bb32c970b0162ff767a9a970d-750wi" style="width: 720px;" title="Jetcontrail by jensloeffel01"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br&gt;&lt;br&gt;&lt;strong&gt;Photographer&lt;/strong&gt;: &lt;a href="mailto:jens.hackmann@freenet.de" target="_self"&gt;Jens Hackmann&lt;/a&gt; &lt;br&gt;&lt;strong&gt;Summary Author&lt;/strong&gt;: &lt;a href="mailto:jens.hackmann@freenet.de" target="_self"&gt;Jens Hackmann&lt;/a&gt;; &lt;a href="mailto:james.l.foster@nasa.gov" target="_self"&gt;Jim Foster&lt;/a&gt;&lt;br&gt;&lt;br&gt;Have you ever looked at a picture you've taken and wondered "How in the world did THAT thing get on my lens?" In this case, the "thing" isn't a turbo-charged worm of some kind but rather an eye-catching jet condensation trail (&lt;a href="http://www.wrh.noaa.gov/fgz/science/contrail.php?wfo=fgz" target="_self"&gt;contrail&lt;/a&gt;). While capturing images of the sunrise over southern Germany about 8:10 January 3, 2012, I couldn't help but notice this odd appearing contrail flying towards the Sun – off the lower left-side of the photo. Contrails take shape when hot, moist air from jet &lt;a href="http://en.wikipedia.org/wiki/Exhaust_gas" target="_self"&gt;exhaust&lt;/a&gt; mixes with the cold ambient air, having a lower &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=vapor-pressure1" target="_self"&gt;vapor pressure&lt;/a&gt; than the exhaust gases. As the exhaust gases cool, they condense into an artificial cloud composed of minute &lt;a href="http://www.sandylandwater.com/slide9.html" target="_self"&gt;water droplets&lt;/a&gt; or &lt;a href="http://www.atoptics.co.uk/halo/crystals.htm" target="_self"&gt;ice crystals&lt;/a&gt;.&lt;br&gt;&lt;br&gt;This contrail and the &lt;a href="http://eo.ucar.edu/webweather/cirrus.html" target="_self"&gt;cirrus deck&lt;/a&gt; above the eastern horizon are sufficiently high, over 30,000 ft (9,150 m), to reflect the dawn’s early light. &lt;a href="http://amsglossary.allenpress.com/glossary/browse?s=w&amp;amp;p=32" target="_self"&gt;Wind shear&lt;/a&gt; to the rear of the jet is responsible for the kink in the contrail. Further behind the jet (top and top center of photo), &lt;a href="http://mysite.du.edu/~etuttle/weather/turbul.htm" target="_self"&gt;atmospheric turbulence&lt;/a&gt; gives the trail its loopy look.&lt;br&gt;&lt;br&gt;&lt;strong&gt;Photo details&lt;/strong&gt;: Camera Maker: Canon; Camera Model: Canon EOS 5D Mark II; Lens: EF100-400mm f/4.5-5.6L IS USM; Focal Length: 400.0mm; Focus Distance: 4294967295.00m; Aperture: f/9.0; Exposure Time: 0.0063 s (1/160); ISO equiv: 100; Exposure Bias: none; Metering Mode: Matrix; Exposure: Manual; Exposure Mode: Manual; White Balance: Auto; Flash Fired: No (enforced); Orientation: Normal; Color Space: sRGB; Software: Adobe Photoshop Camera Raw 6.6 (Windows).&lt;/p&gt;&#xD;
&lt;ul class="related-clicks"&gt;&#xD;
&lt;li class="coords"&gt;Loeffelstelzen, Germany Coordinates: &lt;a href="http://www.panoramio.com/map/#lt=49.508333&amp;amp;ln=9.783611&amp;amp;z=3&amp;amp;k=2" target="_self"&gt;49.508333, 9.783611&lt;/a&gt; &lt;/li&gt;&#xD;
&lt;li class="related"&gt;Related Links             &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2011/03/contrail-confusion.html" target="_self"&gt;Contrail Confusion&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2010/05/contrail-mimicking-rocket-launch.html" target="_self"&gt;Contrail Mimicking Rocket Launch&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://www.nasa.gov/centers/langley/news/factsheets/Windshear.html" target="_self"&gt;Making the Skies Safe from Windshear&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;li class="eo"&gt;Earth Observatory             &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/IOTD/view.php?id=2710" target="_self"&gt;Contrail Web Over the Central Rhone Valley, France&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;/ul&gt;&lt;/div&gt;
&lt;p&gt;&lt;a href="http://feedads.g.doubleclick.net/~a/tI-1LJsQ0yQYFDIzfzmTcrrRpkE/0/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/tI-1LJsQ0yQYFDIzfzmTcrrRpkE/0/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br/&gt;
&lt;a href="http://feedads.g.doubleclick.net/~a/tI-1LJsQ0yQYFDIzfzmTcrrRpkE/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/tI-1LJsQ0yQYFDIzfzmTcrrRpkE/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/EarthSciencePictureOfTheDay/~4/IEFz1I-F-uc" height="1" width="1"/&gt;</content>


    </entry>
    <entry>
        <title>Lake of the Seven Cities</title>
        <link rel="alternate" type="text/html" href="http://epod.usra.edu/blog/2012/01/lake-of-the-seven-cities.html" />
        <link rel="replies" type="text/html" href="http://epod.usra.edu/blog/2012/01/lake-of-the-seven-cities.html" />
        <id>tag:typepad.com,2003:post-6a0105371bb32c970b0162ff59c28e970d</id>
        <published>2012-01-19T03:01:00-05:00</published>
<updated>2012-01-19T03:01:00-05:00</updated>
                <summary>Photographer: Miguel Claro; Miguel's Web site Summary Author: Miguel Claro; Jim Foster The three-photo panorama above features a dormant volcanic crater and the Lake of the Seven Cities on San Miguel Island in the Azore Archipelago. San Miguel is called...</summary>
                        <content type="html" xml:lang="en-US" xml:base="http://epod.usra.edu/blog/">&lt;div xmlns="http://www.w3.org/1999/xhtml"&gt;&lt;p&gt;&lt;a href="http://epod.usra.edu/.a/6a0105371bb32c970b0168e54f4848970c-pi" style="display: inline;"&gt;&lt;img alt="Lagoa7CidadesAtNight-net (3)" class="asset  asset-image at-xid-6a0105371bb32c970b0168e54f4848970c" src="http://epod.usra.edu/.a/6a0105371bb32c970b0168e54f4848970c-750wi" style="width: 720px;" title="Lagoa7CidadesAtNight-net (3)"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br&gt;&lt;br&gt;&lt;strong&gt;Photographer&lt;/strong&gt;: &lt;a href="mailto:miguelclaro@sapo.pt" target="_self"&gt;Miguel Claro&lt;/a&gt;; &lt;a href="http://www.astrosurf.com/astroarte/Lagoa7CidadesAtNight-net.jpg" target="_self"&gt;Miguel's Web site&lt;/a&gt; &lt;br&gt;&lt;strong&gt;Summary Author&lt;/strong&gt;: &lt;a href="mailto:miguelclaro@sapo.pt" target="_self"&gt;Miguel Claro&lt;/a&gt;; &lt;a href="mailto:james.l.foster@nasa.gov" target="_self"&gt;Jim Foster&lt;/a&gt;&lt;br&gt;&lt;br&gt;The three-photo panorama above features a dormant &lt;a href="http://en.wikipedia.org/wiki/Volcanic_crater" target="_self"&gt;volcanic crater&lt;/a&gt; and the &lt;a href="http://en.wikipedia.org/wiki/Lagoa_das_Sete_Cidades" target="_self"&gt;Lake of the Seven Cities&lt;/a&gt; on &lt;a href="http://en.wikipedia.org/wiki/S%C3%A3o_Miguel_Island" target="_self"&gt;San Miguel Island&lt;/a&gt; in the &lt;a href="http://en.wikipedia.org/wiki/Azores" target="_self"&gt;Azore Archipelago&lt;/a&gt;. San Miguel is called the "Green Island" because it's the most verdant and also most populous of the Azores. Though the volcano that formed San Miguel has been extinct for approximately 400 years, its lake-filled &lt;a href="http://volcanoes.usgs.gov/images/pglossary/caldera.php" target="_self"&gt;caldera&lt;/a&gt; is a one of the main sources of fresh water in the &lt;a href="http://education.nationalgeographic.com/education/encyclopedia/archipelago/?ar_a=4&amp;amp;ar_r=1" target="_self"&gt;archipelago&lt;/a&gt; and has thus facilitated the development of a number of population centers. On this nighttime long exposure, &lt;a href="http://www.lrc.rpi.edu/programs/nlpip/lightinganswers/lightpollution/lightPollution.asp" target="_self"&gt;stray light&lt;/a&gt; from the towns surrounding the lake (actually two lakes) and reflecting off the cloud deck gives this scene a yellowish pall. &lt;br&gt;&lt;br&gt;&lt;strong&gt;Photo details&lt;/strong&gt;: Canon 50D camera; ISO 800; F/4; 10mm. Panorama composed of three images taken     &lt;br&gt;at 2:40 a.m. on December 4, 2011; three minute exposure for each photo. Software: Adobe Photoshop CS3 Windows.&lt;/p&gt;&#xD;
&lt;ul class="related-clicks"&gt;&#xD;
&lt;li class="coords"&gt;San Miguel Coordinates: &lt;a href="http://www.panoramio.com/map/#lt=37.754566&amp;amp;ln=-25.308552&amp;amp;z=3&amp;amp;k=2&amp;amp;a=1&amp;amp;tab=1" target="_self"&gt;37.7545, -25.3085&lt;/a&gt; &lt;/li&gt;&#xD;
&lt;li class="related"&gt;Related Links            &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2012/01/phantom-ship-and-crater-lake.html" target="_self"&gt;Phantom Ship and Crater Lake&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;li class="eo"&gt;Earth Observatory            &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/IOTD/view.php?id=45059" target="_self"&gt;Rabaul Caldera&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;/ul&gt;&lt;/div&gt;
&lt;p&gt;&lt;a href="http://feedads.g.doubleclick.net/~a/spIcf5l7rzIEAh27MA2uQWknLlo/0/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/spIcf5l7rzIEAh27MA2uQWknLlo/0/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br/&gt;
&lt;a href="http://feedads.g.doubleclick.net/~a/spIcf5l7rzIEAh27MA2uQWknLlo/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/spIcf5l7rzIEAh27MA2uQWknLlo/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/EarthSciencePictureOfTheDay/~4/YXEc9Zv-ZXE" height="1" width="1"/&gt;</content>


    </entry>
    <entry>
        <title>Mars Observed from a 10-inch Telescope</title>
        <link rel="alternate" type="text/html" href="http://epod.usra.edu/blog/2012/01/mars-observed-from-a-10-inch-telescope.html" />
        <link rel="replies" type="text/html" href="http://epod.usra.edu/blog/2012/01/mars-observed-from-a-10-inch-telescope.html" />
        <id>tag:typepad.com,2003:post-6a0105371bb32c970b0162ff559414970d</id>
        <published>2012-01-18T03:01:00-05:00</published>
<updated>2012-01-18T03:01:00-05:00</updated>
                <summary>Photographer: John Chumack; John’s Web site Summary Author: John Chumack; Jim Foster Mars is now much brighter and closer than it was just a month ago. When this image was acquired on January 5, 2012, Mars was 9.36 arc seconds...</summary>
                        <content type="html" xml:lang="en-US" xml:base="http://epod.usra.edu/blog/">&lt;div xmlns="http://www.w3.org/1999/xhtml"&gt;&lt;p&gt;&lt;a href="http://epod.usra.edu/.a/6a0105371bb32c970b01676067ba2f970b-pi" style="display: inline;"&gt;&lt;img alt="Mars Observed" class="asset  asset-image at-xid-6a0105371bb32c970b01676067ba2f970b" src="http://epod.usra.edu/.a/6a0105371bb32c970b01676067ba2f970b-750wi" style="width: 720px;" title="Mars Observed"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br&gt;&lt;br&gt;&lt;strong&gt;Photographer&lt;/strong&gt;: &lt;a href="mailto:John.Chumack@udri.udayton.edu" target="_self"&gt;John Chumack&lt;/a&gt;; &lt;a href="http://www.galacticimages.com" target="_self"&gt;John’s Web site&lt;/a&gt; &lt;br&gt;&lt;strong&gt;Summary Author&lt;/strong&gt;: &lt;a href="mailto:John.Chumack@udri.udayton.edu" target="_self"&gt;John Chumack&lt;/a&gt;; &lt;a href="mailto:james.l.foster@nasa.gov" target="_self"&gt;Jim Foster&lt;/a&gt;&lt;br&gt;&lt;br&gt;&lt;a href="http://nineplanets.org/mars.html" target="_self"&gt;Mars&lt;/a&gt; is now much brighter and closer than it was just a month ago. When this image was acquired on January 5, 2012, Mars was 9.36 &lt;a href="http://coolcosmos.ipac.caltech.edu/cosmic_classroom/cosmic_reference/angular.html" target="_self"&gt;arc seconds&lt;/a&gt; in diameter, nearly twice the size it appeared in early December. From my backyard observatory near &lt;a href="http://en.wikipedia.org/wiki/Dayton,_Ohio" target="_self"&gt;Dayton, Ohio&lt;/a&gt;, I could easily detect some of the &lt;a href="http://starryskies.com/articles/2004/01/mars.red.html" target="_self"&gt;Red Planet’s&lt;/a&gt; surface features including its &lt;a href="http://www.daviddarling.info/encyclopedia/M/Marspoles.html" target="_self"&gt;north polar cap&lt;/a&gt; – it looked like a Christmas tree ornament hanging in the night sky. Mars is getting closer to us, and sometime between the end of February to the beginning of March it’ll be at its largest (13.8 arc seconds) during this &lt;a href="http://mathdl.maa.org/mathDL/46/?pa=content&amp;amp;sa=viewDocument&amp;amp;nodeId=3120&amp;amp;bodyId=3357" target="_self"&gt;current two-year cycle&lt;/a&gt;. Please don’t think Mars will ever get as big as the &lt;a href="http://www.freemars.org/jeff/planets/Luna/Luna.htm" target="_self"&gt;Moon&lt;/a&gt; appears, as it’s made to look in those &lt;a href="http://science.nasa.gov/science-news/science-at-nasa/2009/09jun_marshoax/" target="_self"&gt;silly images&lt;/a&gt; that circulate every year or so. At its closest approach, it won't look much bigger than it does now. To observe &lt;a href="http://www.nightskyinfo.com/" target="_self"&gt;Mars&lt;/a&gt;, look for it well after nightfall in the eastern sky, near the constellation of &lt;a href="http://www.nightskyinfo.com/maps_images/html/mars_map_mid.htm" target="_self"&gt;Leo&lt;/a&gt;. The shot above was captured with a 10 in (25 cm) telescope on the morning of January 5, 2012 at approximately 7:00.&lt;br&gt;&lt;br&gt;&lt;strong&gt;Photo details&lt;/strong&gt;: 10-inch Meade SCT telescope; DMK 21AF04 fire-wire Camera (640x480); 2x Barlow lens; 3,300 frames stacked in &lt;a href="http://www.astronomie.be/registax/" target="_self"&gt;Registax6&lt;/a&gt;.&lt;/p&gt;&#xD;
&lt;ul class="related-clicks"&gt;&#xD;
&lt;li class="coords"&gt;Yellow Springs, Ohio, Coordinates: &lt;a href="http://www.panoramio.com/map/#lt=39.80167&amp;amp;ln=-83.89278&amp;amp;z=3&amp;amp;k=2" target="_self"&gt;39.80167, -83.89278&lt;/a&gt; &lt;/li&gt;&#xD;
&lt;li class="related"&gt;Related Links            &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2006/05/mars-from-spirit.html" target="_self"&gt;Mars from Spirit&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://epod.usra.edu/blog/2003/08/moon-and-mars-comparison.html" target="_self"&gt;Moon and Mars Comparison&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://www.fourmilab.ch/cgi-bin/Solar/action?sys=-Si" target="_self"&gt;Solar System Live&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;li class="eo"&gt;Earth Observatory            &#xD;
&lt;ul&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/IOTD/view.php?id=3481" target="_self"&gt;Earth and Moon as Viewed from Mars&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;li&gt;&lt;a href="http://earthobservatory.nasa.gov/IOTD/view.php?id=8786" target="_self"&gt;Permafrost on Mars and Earth&lt;/a&gt;&lt;/li&gt;&#xD;
&lt;/ul&gt;&#xD;
&lt;/li&gt;&#xD;
&lt;/ul&gt;&lt;/div&gt;
&lt;p&gt;&lt;a href="http://feedads.g.doubleclick.net/~a/Ik4CJ_JngZjeQex6iOTi1n8pncY/0/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/Ik4CJ_JngZjeQex6iOTi1n8pncY/0/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;br/&gt;
&lt;a href="http://feedads.g.doubleclick.net/~a/Ik4CJ_JngZjeQex6iOTi1n8pncY/1/da"&gt;&lt;img src="http://feedads.g.doubleclick.net/~a/Ik4CJ_JngZjeQex6iOTi1n8pncY/1/di" border="0" ismap="true"&gt;&lt;/img&gt;&lt;/a&gt;&lt;/p&gt;&lt;img src="http://feeds.feedburner.com/~r/EarthSciencePictureOfTheDay/~4/XC0Ipgxs5lw" height="1" width="1"/&gt;</content>


    </entry>

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