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          <TitleText>Carte pédologique de France à 1/100 000</TitleText>
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        <SubjectHeadingText>|Milieux naturels et environnement|Sol;Atlas, cartes et SIG</SubjectHeadingText>
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        <Text language="fre">&lt;p&gt;La carte des sols de Besan&amp;ccedil;on &amp;agrave; 1/100 000 occupe une position centrale dans la r&amp;eacute;gion de Franche-Comt&amp;eacute;. Elle est repr&amp;eacute;sentative de la distribution des sols d&amp;eacute;velopp&amp;eacute;s sur le calcaire jurassique.&lt;/p&gt;</Text>
        <Text language="eng">&lt;p&gt;The 1:100,000 Besan&amp;ccedil;on soil map holds a central position in the Franche-Comt&amp;eacute; region. It is representative of the distribution of soils developed on the Jurassic limestone.&lt;/p&gt;</Text>
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        <Text>La carte des sols de Besançon à 1/100 000 occupe une position centrale dans la région de Franche-Comté. Elle est représentative de la distribution des sols développés sur le calcaire jurassique.</Text>
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        <Text>&lt;p&gt;AVANT-PROPOS&lt;br /&gt;INTRODUCTION&lt;br /&gt;&lt;br /&gt;PREMIERE PARTIE &amp;ndash; GENERALITES&lt;br /&gt;&lt;strong&gt;I - DEFINITION DES UNITES CARTOGRAPHIQUES&lt;/strong&gt;&lt;br /&gt;A. Les crit&amp;egrave;res de d&amp;eacute;finition des unit&amp;eacute;s&amp;nbsp;&amp;nbsp; &amp;nbsp;&lt;br /&gt;1. Les r&amp;eacute;gions naturelles&amp;nbsp;&amp;nbsp; &amp;nbsp;&lt;br /&gt;2. Les crit&amp;egrave;res d&amp;#39;a&amp;eacute;ration ou d&amp;#39;anoxie associ&amp;eacute;s &amp;agrave; la d&amp;eacute;finition des syst&amp;egrave;mes de subsurface&amp;nbsp;&amp;nbsp; &amp;nbsp;&lt;br /&gt;3. La position g&amp;eacute;omorphologique&lt;br /&gt;4. La profondeur rhizofonctionnelle&lt;br /&gt;5. Le mode d&amp;#39;utilisation actuelle des sols&lt;br /&gt;B. Le rattachement aux syst&amp;egrave;mes de classification&lt;br /&gt;&lt;strong&gt;II - LA CARTOGENESE&lt;/strong&gt;&lt;br /&gt;A. Les principes d&amp;rsquo;organisation du milieu naturel&lt;br /&gt;1. La loi des &amp;quot;compartiments&amp;quot;&lt;br /&gt;2. La loi des &amp;quot;buttes&amp;quot;&lt;br /&gt;3. La loi des &amp;quot;cha&amp;icirc;nes de sols&amp;quot;&lt;br /&gt;B. R&amp;eacute;alisation pratique des cartes de Besan&amp;ccedil;on, Quingey et Ornans&lt;br /&gt;1. La phase pr&amp;eacute;paratoire&lt;br /&gt;2. La phase de prospection de terrain&lt;br /&gt;3. La phase de dessin de la carte&lt;br /&gt;4. La phase de contr&amp;ocirc;le&lt;br /&gt;C. R&amp;eacute;alisation de la carte de Vercel &amp;agrave; 1/50 000&amp;nbsp;&amp;nbsp; &amp;nbsp;26&lt;br /&gt;1. M&amp;eacute;thodologie&lt;br /&gt;2. Le changement d&amp;#39;&amp;eacute;chelle et la repr&amp;eacute;sentation cartographique&lt;br /&gt;D. Synth&amp;egrave;se au 1/100 000&lt;br /&gt;1. Cartes de Besan&amp;ccedil;on, Quingey, Ornans&lt;br /&gt;2. Carte de Vercel&lt;br /&gt;3. La base de donn&amp;eacute;es associ&amp;eacute;e&lt;br /&gt;&lt;strong&gt;III - LE TERRITOIRE DE LA CARTE&lt;/strong&gt;&lt;br /&gt;A. Situation administrative, g&amp;eacute;ographique et climatique&lt;br /&gt;B. Les r&amp;eacute;gions naturelles&lt;br /&gt;1. Les plateaux de basse et de moyenne altitude&lt;br /&gt;2. Le deuxi&amp;egrave;me plateau et la montagne&lt;br /&gt;3. Les faisceaux et recul&amp;eacute;es&lt;br /&gt;4. Les vall&amp;eacute;es du Doubs et de la Loue&lt;br /&gt;5. La vall&amp;eacute;e de l&amp;#39;Ognon et les terrasses anciennes de Chaux&lt;br /&gt;&lt;br /&gt;DEUXIEME PARTIE &amp;ndash; LES SOLS&lt;br /&gt;&lt;strong&gt;IV - LES PLATEAUX DE BASSE ET DE MOYENNE ALTITUDE&lt;/strong&gt;&lt;br /&gt;A. Les sols a&amp;eacute;r&amp;eacute;s sur roches fractur&amp;eacute;es&lt;br /&gt;1. Position topographique sommitale (formes convexes ou planes)&lt;br /&gt;2. Position topographique de d&amp;eacute;pression (formes concaves)&lt;br /&gt;3. Associations de sols a&amp;eacute;r&amp;eacute;s des formes convexes ou planes&lt;br /&gt;B. Sols anoxiques sur roches non fractur&amp;eacute;es&lt;br /&gt;1. Position topographique sommitale (formes convexes ou planes)&lt;br /&gt;2. Position de d&amp;eacute;pression (vallons &amp;agrave; ruisseau permanent ou temporaire)&lt;br /&gt;C. Associations de sols anoxiques sur substratum non fractur&amp;eacute;&lt;br /&gt;&lt;strong&gt;V - LE DEUXIEME PLATEAU ET LA MONTAGNE&lt;/strong&gt;&lt;br /&gt;A. Sols a&amp;eacute;r&amp;eacute;s sur roches fractur&amp;eacute;es&lt;br /&gt;1. Position topographique sommitale (formes convexes ou planes)&lt;br /&gt;2. Position topographique variable (sommets, pentes &amp;lt; 25 %)&lt;br /&gt;B. Association des sols a&amp;eacute;r&amp;eacute;s sur roches fractur&amp;eacute;es&lt;br /&gt;1. Position topographique sommitale (formes convexes ou planes)&lt;br /&gt;2. Position topographique variable (sommets, replats, pentes &amp;lt;25%)&lt;br /&gt;C. Association de sols anoxiques&lt;br /&gt;&lt;strong&gt;VI - LES FAISCEAUX PLISSES ET LES RECULEES&lt;/strong&gt;&lt;br /&gt;A. Position topographique sommitale (formes convexes ou planes)&amp;nbsp;&amp;nbsp; &amp;nbsp;&lt;br /&gt;B. Association de sols a&amp;eacute;r&amp;eacute;s acides de position sommitale et de d&amp;eacute;pression&lt;br /&gt;C. Pentes tr&amp;egrave;s fortes (&amp;gt; 50 %), front des bancs&lt;br /&gt;D. Associations de sols de pentes tr&amp;egrave;s fortes&lt;br /&gt;&lt;strong&gt;VII - LES VALLEES DE LA LOUE ET DU DOUBS&lt;/strong&gt;&lt;br /&gt;A. Sols a&amp;eacute;r&amp;eacute;s des alluvions &amp;agrave; nappe phr&amp;eacute;atique libre&lt;br /&gt;1. Terrasses r&amp;eacute;centes du lit majeur&lt;br /&gt;2. Transition coteaux &amp;ndash; terrasses&lt;br /&gt;3. Terrasses de la zone de divagation des eaux&lt;br /&gt;B. Association des sols anoniques &amp;ndash; terrasses de la zone de divagation des eaux&amp;nbsp;&amp;nbsp; &amp;nbsp;&lt;br /&gt;&lt;strong&gt;VIII - PLAINE DE L&amp;rsquo;OGNON ET TERRASSES ANCIENNES DE CHAUX&lt;/strong&gt;&lt;br /&gt;A. Sols a&amp;eacute;r&amp;eacute;s&lt;br /&gt;1. Sols des terrasses r&amp;eacute;centes, profonds ou moyennement profonds&lt;br /&gt;2. Sols des terrasses anciennes, talus &amp;eacute;rod&amp;eacute;s, cailloutis&lt;br /&gt;B. Sols anoxiques&lt;br /&gt;1. Sols des terrasses r&amp;eacute;centes&lt;br /&gt;2. Sols des terrasses anciennes&lt;br /&gt;&lt;br /&gt;CONCLUSIONS&lt;br /&gt;ANNEXES&lt;br /&gt;&amp;nbsp;&lt;/p&gt;</Text>
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