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    <channel>        <title>Favorite National parks</title>
        <description>Album by 1pp5o4ie674vq on The Apple Corps</description>
        <link>http://applecorp.ning.com/photo/albums/2058425:Album:1685</link>
        <pubDate>Sat, 26 Dec 2009 19:17:09 +0000</pubDate>
        <lastBuildDate>Sat, 26 Dec 2009 19:17:09 +0000</lastBuildDate>
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            <title>Favorite National parks</title>
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                        	<guid>2058425:Photo:1152</guid>             <title>Mount Gould and Angel Wing, Glacier National Park, Montana. 2002</title>
            <link>http://applecorp.ning.com/photo/2058425:Photo:1152</link>
                            <description>&lt;a href=&quot;http://api.ning.com/files/Xn1MqnTOOfXyn-5GTgrHtP5lyizvUGaLDyXcDM1NProYK*7mZSBN9xuEIgVuJmGN-c-0iRZQPoNFVd*UcM3YSRBgjy0xRa4C/1060684_IMG.jpg?width=640&amp;amp;height=480&quot;&gt;&lt;img src=&quot;http://api.ning.com/files/Xn1MqnTOOfXyn-5GTgrHtP5lyizvUGaLDyXcDM1NProYK*7mZSBN9xuEIgVuJmGN-c-0iRZQPoNFVd*UcM3YSRBgjy0xRa4C/1060684_IMG.jpg?width=240&amp;height=180&quot;&gt;&lt;/a&gt;
                
            by Ed Waldrup This is the post card view from the Many Glacier Hotel area. The dark horizontal band of igneous rock ( Purcell Sill ) on Mt. Gould is diorite. Sills are formed when magma forces its way in between layers of sedimentary rock and then hardens. Throughout most of the park, the sill stands out as a 130 to 300 ft. dark layer of diorite sandwiched between strips of white, low-grade marble that formed as heat from the cooling magma baked the limestone. This heat also drove out organic material, bleaching the rock and causing more contrast between the darker diorite and the marble. Since the sill was injected after the sedimentary layers were deposited, geologists can’t simply say the layers above it are younger than it and those below are older than the sill. Nonetheless, when geologists see it they know they are looking at the Helena (Siyeh) Formation, which lies just above the older rocks of the Empire Formation, and just below the younger rocks of the Snowslip Formation.Height of Mount Gould is 9550 ft. The only through road, Going to the Sun Road is normally plowed by end of June and is on the other side of Gould on the Continental Divide.</description>
                <pubDate>Sun, 29 Jun 2008 17:55:57 +0000</pubDate>
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            	            <media:description>This is the post card view from the Many Glacier Hotel area. The dark horizontal band of igneous rock ( Purcell Sill ) on Mt. Gould is diorite. Sills are formed when magma forces its way in between layers of sedimentary rock and then hardens. Throughout most of the park, the sill stands out as a 130 to 300 ft. dark layer of diorite sandwiched between strips of white, low-grade marble that formed as heat from the cooling magma baked the limestone. This heat also drove out organic material, bleaching the rock and causing more contrast between the darker diorite and the marble. Since the sill was injected after the sedimentary layers were deposited, geologists can’t simply say the layers above it are younger than it and those below are older than the sill. Nonetheless, when geologists see it they know they are looking at the Helena (Siyeh) Formation, which lies just above the older rocks of the Empire Formation, and just below the younger rocks of the Snowslip Formation.Height of Mount Gould is 9550 ft. The only through road, Going to the Sun Road is normally plowed by end of June and is on the other side of Gould on the Continental Divide.</media:description>
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	            <media:credit role="photographer">Ed Waldrup</media:credit>
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                        	<guid>2058425:Photo:1151</guid>             <title>Bearhat Mountain, Glacier National Park, Montana 2004</title>
            <link>http://applecorp.ning.com/photo/2058425:Photo:1151</link>
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            by Ed Waldrup Hidden Lake is at the base of 8684 ft. Bearhat mountain. This overlook is easily hikeable from the visitors center at Logan Pass. The Continental Divide goes through this area. The mountain is named for a Kootenai tribal leader.</description>
                <pubDate>Sun, 29 Jun 2008 17:55:55 +0000</pubDate>
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            	            <media:description>Hidden Lake is at the base of 8684 ft. Bearhat mountain. This overlook is easily hikeable from the visitors center at Logan Pass. The Continental Divide goes through this area. The mountain is named for a Kootenai tribal leader.</media:description>
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	            <media:credit role="photographer">Ed Waldrup</media:credit>
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                        	<guid>2058425:Photo:1147</guid>             <title>2002. Helicopter shot of Triple Divide Peak, Glacier National Park, Montana. 8020 ft.</title>
            <link>http://applecorp.ning.com/photo/2002-helicopter-shot-of-triple</link>
                            <description>&lt;a href=&quot;http://api.ning.com/files/-Vyo*ygZO0bIeyXEEhl1yp55XabQlSi7ngIAUZWxxgllFg2aIAxmzB8hdcNiV8WkMo4i9RsczDdscNnDRMmJPMU7APr6rvSG/TrippleDividePeak.jpg?width=640&amp;amp;height=437&quot;&gt;&lt;img src=&quot;http://api.ning.com/files/-Vyo*ygZO0bIeyXEEhl1yp55XabQlSi7ngIAUZWxxgllFg2aIAxmzB8hdcNiV8WkMo4i9RsczDdscNnDRMmJPMU7APr6rvSG/TrippleDividePeak.jpg?width=240&amp;height=163&quot;&gt;&lt;/a&gt;
                
            by Ed Waldrup Shot on Fuji Velvia film. Canon EOS1v. Triple Divide Peak is a hydrologic apex of the North American continent. The waters from this peak flow into three major drainages: the Hudson&#039;s Bay, through the St. Mary and Saskatchewan; the Pacific, through the Flathead and Columbia; and the Gulf of Mexico, through the Missouri-Mississippi.</description>
                <pubDate>Sun, 29 Jun 2008 17:15:37 +0000</pubDate>
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            	            <media:description>Shot on Fuji Velvia film. Canon EOS1v. Triple Divide Peak is a hydrologic apex of the North American continent. The waters from this peak flow into three major drainages: the Hudson&#039;s Bay, through the St. Mary and Saskatchewan; the Pacific, through the Flathead and Columbia; and the Gulf of Mexico, through the Missouri-Mississippi.</media:description>
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	            <media:credit role="photographer">Ed Waldrup</media:credit>
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                        	<guid>2058425:Photo:1145</guid>             <title>1983 Grand Canyon</title>
            <link>http://applecorp.ning.com/photo/2058425:Photo:1145</link>
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            by Ed Waldrup When we first arrived at the Grand Canyon I started shooting photos in the middle, of the day. The better time, I learned is at dusk or dawn. Photographers know this as the Golden Hour.</description>
                <pubDate>Sun, 29 Jun 2008 17:05:16 +0000</pubDate>
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            	            <media:description>When we first arrived at the Grand Canyon I started shooting photos in the middle, of the day. The better time, I learned is at dusk or dawn. Photographers know this as the Golden Hour.</media:description>
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	            <media:credit role="photographer">Ed Waldrup</media:credit>
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