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+<html >
+<head >
+<title >Moon</title>
+</head>
+
+<body >
+<mbp:pagebreak/>
+<tei-ms:entry>
+<tei-ms:orth><h1 align="center" >Moon</h1></tei-ms:orth>
+</tei-ms:entry>
+
+<br />
+<div align="center" title="The only object apart from Earth mankind ever stood on."><img src="moon.jpg"  /></div>
+<p ><b class="first" >A</b> lthough most known planets have many moons or
+satellites, the <a href="earth.htm">Earth</a>’s own Moon has been studied in the most detail with his
+close proximity. The Moon is one-fourth the size of <a href="earth.htm"> Earth</a> and so the pull of
+gravity on the lunar surface is approximately one-sixth of that on <a href="earth.htm">Earth</a>.</p>
+<p >Recent expeditions, mainly by the satellite Clementine have led to the
+discovery of a frozen ice formations at the poles of the Moon; however, the Moon
+does not have free water nor an atmosphere, which causes a static state of
+weather.</p>
+<p >Revolving about the <a href="earth.htm"> Earth</a> approximately every 27 days, the Moon is 384,403 km
+(238,857 mi).</p>
+<p >While the origin of our companion Moon remains in debate, the most probably
+theory of formation is the planetesimal impact. Stated within this theory is
+that the Moon originally grew from the dust particles of an original nebulae
+that formed the <a href="earth.htm"> Earth</a> and the rest of the Solar System.</p>
+<p >As the <a href="earth.htm"> Earth</a> had begun its first rotations, the Moon spun off and because of
+its smaller mass, it was grabbed by gravitation into eternal revolution about
+the <a href="earth.htm">Earth</a>. This theory has been repeatedly been proven by the similarity between
+the densities of the <a href="earth.htm">Earth</a>’s upper crust rocks and Moon rocks.</p>
+<p >Still, with NASA budget cuts, missions to our closest neighbor have become
+rare, leaving many Moon colonization plans to be canceled.</p>
+
+</body>
+
+</html>