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	<title>ExpOOs / Maison des Min&#233;raux</title>
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<item xml:lang="en">
		<title>The arch </title>
		<link>https://expoos.mmx.bzh/article762.html</link>
		<guid isPermaLink="true">https://expoos.mmx.bzh/article762.html</guid>
		<dc:date>2025-07-02T09:58:56Z</dc:date>
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		<dc:language>en</dc:language>
		<dc:creator>rgilbert</dc:creator>



		<description>
&lt;p&gt;Rock: granite Type: plutonic igneous rock Age: 300 Ma Quarry: Le Houx in Langu&#233;dias (C&#244;tes d'Armor) &lt;br class='autobr' /&gt;
A Fine Granite &lt;br class='autobr' /&gt;
This granite, with a fine texture, is composed of feldspars (plagioclase, microcline), quartz, muscovite (white mica), and a bit of biotite (black mica). Along with its neighbor, the Hingl&#233; granite, it belongs to a large batholith (from the Greek &#8220;bathos&#8221; meaning depth and &#8220;lithos&#8221; meaning rock), the Bobital-Dinan massif, formed during the Variscan (Hercynian) orogeny. (&#8230;)&lt;/p&gt;


-
&lt;a href="https://expoos.mmx.bzh/rubrique39.html" rel="directory"&gt;Curious Breton garden&lt;/a&gt;


		</description>


 <content:encoded>&lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L150xH100/img_8194_niv_languedias_collection_mmx-3-8fde9.jpg?1751515184' class='spip_logo spip_logo_right' width='150' height='100' alt=&#034;&#034; /&gt;
		&lt;div class='rss_texte'&gt;&lt;blockquote class=&#034;spip&#034;&gt;
&lt;p&gt; &lt;strong&gt;Rock&lt;/strong&gt;: granite &lt;br class='autobr' /&gt;
&lt;strong&gt;Type&lt;/strong&gt;: plutonic igneous rock &lt;br class='autobr' /&gt;
&lt;strong&gt;Age&lt;/strong&gt;: 300 Ma &lt;br class='autobr' /&gt;
&lt;strong&gt;Quarry&lt;/strong&gt;: Le Houx in Langu&#233;dias (C&#244;tes d'Armor)&lt;/p&gt;
&lt;/blockquote&gt;&lt;h2 class=&#034;spip&#034;&gt;A Fine Granite&lt;/h2&gt;
&lt;p&gt;This granite, with a fine texture, is composed of feldspars (plagioclase, microcline), quartz, muscovite (white mica), and a bit of biotite (black mica). Along with its neighbor, the Hingl&#233; granite, it belongs to a large batholith (from the Greek &#8220;bathos&#8221; meaning depth and &#8220;lithos&#8221; meaning rock), the Bobital-Dinan massif, formed during the Variscan (Hercynian) orogeny.&lt;/p&gt;
&lt;h2 class=&#034;spip&#034;&gt;Granite with or without an &#8220;e&#8221;?&lt;/h2&gt;
&lt;p&gt;Two spellings, two meanings. &#8220;Granit&#8221; (without an &#8220;e&#8221;) is a commercial term used by the extractive industry and refers to a hard, coarse-grained rock. &#8220;Granite&#8221; (with an &#8220;e&#8221;) is the term geologists use to name this plutonic igneous rock. This means that a &#8220;granit&#8221; does not necessarily mean &#8220;granite&#8221;! For example, the &#8220;petit granit&#8221; of the Ardennes refers to a limestone, a sedimentary rock.&lt;/p&gt;
&lt;h2 class=&#034;spip&#034;&gt;Forming and quarrying&lt;/h2&gt;
&lt;p&gt;The elements of this arch were prepared by young stonemasons from the Apprentice Training Center (CFA) of UNICEM, located in Louvign&#233;-du-D&#233;sert, about 70 kilometers north of Rennes (Ille-et-Vilaine). This Brittany campus benefits from a training site equipped with state-of-the-art teaching tools. Today, four programs are offered: quarry equipment maintenance, public works and handling machinery mechanics, laboratory technician, and finally, stone-cutting trades.&lt;/p&gt;
&lt;div class='spip_document_425 spip_document spip_documents spip_document_image spip_documents_center spip_document_center spip_document_avec_legende' data-legende-len=&#034;77&#034; data-legende-lenx=&#034;xx&#034;
&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/jpg/graphic-node-ea0geeigsou-unsplash_cadrage.jpg' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/jpeg&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH470/graphic-node-ea0geeigsou-unsplash_cadrage-28235.jpg?1680580015' width='500' height='470' alt='' /&gt;&lt;/a&gt;
&lt;figcaption class='spip_doc_legende'&gt; &lt;div class='spip_doc_credits crayon document-credits-425 '&gt;graphicnode - arche / Unsplash / &lt;a href=&#034;https://unsplash.com/fr/photos/EA0gEEIGsoU&#034; class=&#034;spip_url spip_out auto&#034; rel=&#034;nofollow external&#034;&gt;https://unsplash.com/fr/photos/EA0gEEIGsoU&lt;/a&gt;
&lt;/div&gt;
&lt;/figcaption&gt;&lt;/figure&gt;
&lt;/div&gt;&lt;h2 class=&#034;spip&#034;&gt;A Breton Gem&lt;/h2&gt;
&lt;p&gt;Granite is marketed under two names: &#8220;gris perle&#8221; (pearl gray) and &#8220;beige de Langu&#233;dias.&#8221; These color variations depend on the degree of rock alteration. The beige is slightly altered, while the gray is sound. The &#8220;Langu&#233;dias&#8221; quarry has been heavily exploited. It has the highest quarry density in Brittany and has been worked since the late 19th century. Granite was primarily used for paving stones for roadways and is now notably featured on the floor of the Cour Napol&#233;on at the Grand Louvre in Paris.&lt;/p&gt;
&lt;div class='spip_document_358 spip_document spip_documents spip_document_image spip_documents_center spip_document_center spip_document_avec_legende' data-legende-len=&#034;129&#034; data-legende-lenx=&#034;xxx&#034;
&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/jpg/paris_75001_cour_napoleon_louvre_aile_turgot_02b_20141107_125236.jpg' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/jpeg&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH281/paris_75001_cour_napoleon_louvre_aile_turgot_02b_20141107_125236-e578e.jpg?1680580015' width='500' height='281' alt='' /&gt;&lt;/a&gt;
&lt;figcaption class='spip_doc_legende'&gt; &lt;div class='spip_doc_credits crayon document-credits-358 '&gt;Nathanael Burton / Wikimedia Commons / CC BY-SA 2.0 / File:Paris 75001 Cour Napol&#233;on Louvre Aile Turgot 02b 20141107 125236.jpg
&lt;/div&gt;
&lt;/figcaption&gt;&lt;/figure&gt;
&lt;/div&gt;&lt;/div&gt;
		
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<item xml:lang="en">
		<title>Nodule</title>
		<link>https://expoos.mmx.bzh/article222.html</link>
		<guid isPermaLink="true">https://expoos.mmx.bzh/article222.html</guid>
		<dc:date>2023-06-29T10:49:26Z</dc:date>
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		<dc:language>en</dc:language>
		<dc:creator>amenez, Google Translate</dc:creator>



		<description>
&lt;p&gt;Silurian nodule (-410 million years) from black shales located in Argol. The iron oxides in visible surface of the sample indicate the presence of pyrite. This nodule in the exhibition are the biggest concretion discovered in Crozon Peninsula .&lt;/p&gt;


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&lt;a href="https://expoos.mmx.bzh/rubrique5.html" rel="directory"&gt;Geology of &#034;La presqu'&#238;le de Crozon&#034;&lt;/a&gt;


		</description>


 <content:encoded>&lt;div class='rss_texte'&gt;&lt;p&gt;Silurian nodule (-410 million years) from black shales located in Argol. The iron oxides in visible surface of the sample indicate the presence of pyrite. This nodule in the exhibition are the biggest concretion discovered in Crozon Peninsula .&lt;/p&gt;&lt;/div&gt;
		
		</content:encoded>


		

	</item>
<item xml:lang="en">
		<title>Pillow lava</title>
		<link>https://expoos.mmx.bzh/article487.html</link>
		<guid isPermaLink="true">https://expoos.mmx.bzh/article487.html</guid>
		<dc:date>2023-06-29T10:34:29Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>en</dc:language>
		<dc:creator>mcleaud</dc:creator>



		<description>
&lt;p&gt;This pillow lava testifies to a period of underwater volcanic activity in the Crozon Peninsula -448 million years ago.&lt;/p&gt;


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&lt;a href="https://expoos.mmx.bzh/rubrique5.html" rel="directory"&gt;Geology of &#034;La presqu'&#238;le de Crozon&#034;&lt;/a&gt;


		</description>


 <content:encoded>&lt;div class='rss_texte'&gt;&lt;p&gt;This pillow lava testifies to a period of underwater volcanic activity in the Crozon Peninsula -448 million years ago.&lt;/p&gt;&lt;/div&gt;
		
		</content:encoded>


		

	</item>
<item xml:lang="en">
		<title>Rhythmic graded breccia</title>
		<link>https://expoos.mmx.bzh/article486.html</link>
		<guid isPermaLink="true">https://expoos.mmx.bzh/article486.html</guid>
		<dc:date>2023-06-29T10:26:51Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>en</dc:language>
		<dc:creator>mcleaud</dc:creator>



		<description>
&lt;p&gt;This rock corresponds to the fallout of volcanic products in the marine environment classified according to their size (grading).
&lt;br class='autobr' /&gt;
The black volcanic particles are cemented by a white limestone matrix.&lt;/p&gt;


-
&lt;a href="https://expoos.mmx.bzh/rubrique5.html" rel="directory"&gt;Geology of &#034;La presqu'&#238;le de Crozon&#034;&lt;/a&gt;


		</description>


 <content:encoded>&lt;div class='rss_texte'&gt;&lt;p&gt;This rock corresponds to the fallout of volcanic products in the marine environment classified according to their size (grading).&lt;br class='autobr' /&gt;
The black volcanic particles are cemented by a white limestone matrix.&lt;/p&gt;&lt;/div&gt;
		
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	</item>
<item xml:lang="en">
		<title>Geode</title>
		<link>https://expoos.mmx.bzh/article475.html</link>
		<guid isPermaLink="true">https://expoos.mmx.bzh/article475.html</guid>
		<dc:date>2022-07-07T20:15:18Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>en</dc:language>
		<dc:creator>amenez</dc:creator>



		<description>
&lt;p&gt;Stone : quartz Type : mineral Age : 304 million years Quarry : Kergantic, Ploemeur (Morbihan) &lt;br class='autobr' /&gt;
Quartz &lt;br class='autobr' /&gt;
This geode features beautiful quartz crystals. It comes from a large vein located in the Kergantic quarry, where kaolin, a white clay, is extracted. Quartz is the most abundant mineral in the continental crust and is composed of silicon and oxygen (SiO&#8322;). It is known for its high resistance to weathering. &lt;br class='autobr' /&gt;
Kaolin: The Product of Granite Leaching &lt;br class='autobr' /&gt;
Kaolin mainly forms from the alteration (&#8230;)&lt;/p&gt;


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&lt;a href="https://expoos.mmx.bzh/rubrique39.html" rel="directory"&gt;Curious Breton garden&lt;/a&gt;


		</description>


 <content:encoded>&lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L150xH100/img_8066_courbes_geode-2-031d5.jpg?1680270100' class='spip_logo spip_logo_right' width='150' height='100' alt=&#034;&#034; /&gt;
		&lt;div class='rss_texte'&gt;&lt;blockquote class=&#034;spip&#034;&gt;
&lt;p&gt;
&lt;strong&gt;Stone&lt;/strong&gt; : quartz&lt;br class='autobr' /&gt;
&lt;strong&gt;Type&lt;/strong&gt; : mineral&lt;br class='autobr' /&gt;
&lt;strong&gt;Age&lt;/strong&gt; : 304 million years&lt;br class='autobr' /&gt;
&lt;strong&gt;Quarry&lt;/strong&gt; : Kergantic, Ploemeur (Morbihan)&lt;/p&gt;
&lt;/blockquote&gt;&lt;h2 class=&#034;spip&#034;&gt;Quartz&lt;/h2&gt;
&lt;p&gt;This geode features beautiful quartz crystals. It comes from a large vein located in the Kergantic quarry, where kaolin, a white clay, is extracted. Quartz is the most abundant mineral in the continental crust and is composed of silicon and oxygen (SiO&#8322;). It is known for its high resistance to weathering.&lt;/p&gt;
&lt;h2 class=&#034;spip&#034;&gt;Kaolin: The Product of Granite Leaching&lt;/h2&gt;
&lt;p&gt;Kaolin mainly forms from the alteration of feldspar-rich rocks, such as granite. Granite is composed of quartz, micas, and feldspars. Feldspars are particularly vulnerable and transform into clay minerals. This transformation is driven by the circulation of hydrothermal fluids ( 550&#176;C) through fractures in the granite massif near the end of its emplacement. The silica released during this process is what forms large quartz veins. Later, about 38 million years ago, Brittany's tropical climate intensified the kaolinization of the massif.&lt;/p&gt;
&lt;h2 class=&#034;spip&#034;&gt;Blank Page and Ceramics&lt;/h2&gt;
&lt;p&gt;Kaolin is used in a wide range of industries. It is a key ingredient in paper production, ceramics, rubber, paint, certain plastics, fiberglass, and more. The first porcelains were made in China 1,800 years ago, using white clay from a &#034;high hill&#034; &#8212; Kao Ling in Chinese.&lt;/p&gt;
&lt;div class='spip_document_410 spip_document spip_documents spip_document_image spip_documents_center spip_document_center spip_document_avec_legende' data-legende-len=&#034;116&#034; data-legende-lenx=&#034;xx&#034;
&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/png/henriot_quimper7_niv.png' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/png&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH479/henriot_quimper7_niv-d78db.png?1680688497' width='500' height='479' alt='' /&gt;&lt;/a&gt;
&lt;figcaption class='spip_doc_legende'&gt; &lt;div class='spip_doc_titre crayon document-titre-410 '&gt;&lt;strong&gt;Fa&#239;ence de Quimper sign&#233;e Henriot (vers 1910)
&lt;/strong&gt;&lt;/div&gt; &lt;div class='spip_doc_credits crayon document-credits-410 '&gt;Patrick.charpiat / Wikimedia Commons / CC BY-3.0 / File:Quimper7.JPG
&lt;/div&gt;
&lt;/figcaption&gt;&lt;/figure&gt;
&lt;/div&gt;&lt;h2 class=&#034;spip&#034;&gt;France's Largest Kaolin Deposit&lt;/h2&gt;
&lt;p&gt;Kaolin from Ploemeur has been mined since 1904, and it is the largest deposit in France. The operating company, Imerys, extracts 60,000 tonnes of kaolin per year. From 1 tonne of raw material, you get approximately:&lt;/p&gt;
&lt;ul class=&#034;spip&#034; role=&#034;list&#034;&gt;&lt;li&gt; 250 kg of kaolin (one quarter)&lt;/li&gt;&lt;li&gt; 50 kg of white micas&lt;/li&gt;&lt;li&gt; 550 kg of quartz-rich sands&lt;br class='autobr' /&gt;
Besides Brittany, kaolin deposits have been or are also mined in Dr&#244;me and Allier departments of France.&lt;/li&gt;&lt;/ul&gt;&lt;div class='spip_document_411 spip_document spip_documents spip_document_image spip_documents_center spip_document_center spip_document_avec_legende' data-legende-len=&#034;85&#034; data-legende-lenx=&#034;xx&#034;
&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/png/vue-aerienne-carriere-kergantic_niv.png' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/png&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH312/vue-aerienne-carriere-kergantic_niv-908fa.png?1680688497' width='500' height='312' alt='' /&gt;&lt;/a&gt;
&lt;figcaption class='spip_doc_legende'&gt; &lt;div class='spip_doc_titre crayon document-titre-411 '&gt;&lt;strong&gt;Vue a&#233;rienne de la carri&#232;re de Kergantic &#224; Ploemeur
&lt;/strong&gt;&lt;/div&gt; &lt;div class='spip_doc_credits crayon document-credits-411 '&gt;fonds IGN / M&#233;galis de Bretagne
&lt;/div&gt;
&lt;/figcaption&gt;&lt;/figure&gt;
&lt;/div&gt;&lt;/div&gt;
		
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<item xml:lang="en">
		<title>Paths</title>
		<link>https://expoos.mmx.bzh/article473.html</link>
		<guid isPermaLink="true">https://expoos.mmx.bzh/article473.html</guid>
		<dc:date>2022-07-07T20:15:15Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>en</dc:language>
		<dc:creator>amenez</dc:creator>



		<description>
&lt;p&gt;Stone : sand Type : sediment Age : between 7 and 3.5 million years Quarry : &#034;Carri&#232;re du Moulin&#034;, Radenac (Morbihan) &lt;br class='autobr' /&gt; Stone : red siltite Type : metamorphic rock Age : 480 millions years Quarry : &#034;Carri&#232;re de Tr&#233;ko&#235;t&#034;, Muel (Ille-et-Vilaine) &lt;br class='autobr' /&gt;
Sand: A Highly Sought-After Material &lt;br class='autobr' /&gt;
The sands of Radenac have been exploited since the early 20th century. These river sands are highly valued for making concrete. Every year, humanity consumes over 50 billion tonnes of sand (80% of which is used (&#8230;)&lt;/p&gt;


-
&lt;a href="https://expoos.mmx.bzh/rubrique39.html" rel="directory"&gt;Curious Breton garden&lt;/a&gt;


		</description>


 <content:encoded>&lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L150xH100/chemins-dsc_0278-2-d200e.jpg?1680270100' class='spip_logo spip_logo_right' width='150' height='100' alt=&#034;&#034; /&gt;
		&lt;div class='rss_texte'&gt;&lt;blockquote class=&#034;spip&#034;&gt;
&lt;p&gt;
&lt;strong&gt;Stone&lt;/strong&gt; : sand&lt;br class='autobr' /&gt;
&lt;strong&gt;Type&lt;/strong&gt; : sediment&lt;br class='autobr' /&gt;
&lt;strong&gt;Age&lt;/strong&gt; : between 7 and 3.5 million years&lt;br class='autobr' /&gt;
&lt;strong&gt;Quarry&lt;/strong&gt; : &#034;Carri&#232;re du Moulin&#034;, Radenac (Morbihan)&lt;/p&gt;
&lt;/blockquote&gt;&lt;blockquote class=&#034;spip&#034;&gt;
&lt;p&gt;
&lt;strong&gt;Stone&lt;/strong&gt; : red siltite&lt;br class='autobr' /&gt;
&lt;strong&gt;Type&lt;/strong&gt; : metamorphic rock&lt;br class='autobr' /&gt;
&lt;strong&gt;Age&lt;/strong&gt; : 480 millions years&lt;br class='autobr' /&gt;
&lt;strong&gt;Quarry&lt;/strong&gt; : &#034;Carri&#232;re de Tr&#233;ko&#235;t&#034;, Muel (Ille-et-Vilaine)&lt;/p&gt;
&lt;/blockquote&gt;&lt;h2 class=&#034;spip&#034;&gt;Sand: A Highly Sought-After Material&lt;/h2&gt;
&lt;p&gt;The sands of Radenac have been exploited since the early 20th century. These river sands are highly valued for making concrete. Every year, humanity consumes over 50 billion tonnes of sand (80% of which is used for concrete production). That's equivalent to a one-meter-thick layer of sand spread across all of Brittany. Sand is the second most-used material on Earth, after water.&lt;/p&gt;
&lt;h2 class=&#034;spip&#034;&gt;The Red Siltstone of Muel&lt;/h2&gt;
&lt;p&gt;The Muel quarry is operated by the company Pomp&#233;i, a public works firm based in Brittany for over 100 years. Opened in 1948, the quarry mainly supplies aggregates for roadworks. It is still active today. Geologically, these siltstones belong to the Pont-R&#233;an Schist Formation (see installation 12).&lt;/p&gt;
&lt;h2 class=&#034;spip&#034;&gt;In an Abandoned Ria&lt;/h2&gt;
&lt;p&gt;The &#034;red sands&#034; extracted at Radenac are ancient sedimentary deposits laid down in the bed of a deep valley near an estuary (a ria or aber). Their presence at over 80 meters in elevation reveals fluctuations in sea level, and therefore, climatic changes. Similar deposits from the same period crop out in other parts of the Armorican Massif. At that time, the island of Brittany (yes, it was once an island) enjoyed a humid subtropical climate, much like Florida today.&lt;/p&gt;
&lt;div class='spip_document_407 spip_document spip_documents spip_document_image spip_documents_center spip_document_center'&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/png/carte_sables_rouges_massif_armoricain.png' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/png&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH500/carte_sables_rouges_massif_armoricain-195d8.png?1680688496' width='500' height='500' alt='' /&gt;&lt;/a&gt;
&lt;/figure&gt;
&lt;/div&gt;&lt;h2 class=&#034;spip&#034;&gt;Sand, Solar Panels: Silicon, My Love&lt;/h2&gt;
&lt;p&gt;This quarry is no longer active and will not be reopened &#8212; the resource is depleted. A landscape, ecological, and agricultural redevelopment project is under consideration, which also includes plans for a solar power plant. Truly, silicon is everywhere: it forms the quartz grains in sand and the cells of solar panels.&lt;/p&gt;
&lt;div class='spip_document_408 spip_document spip_documents spip_document_image spip_documents_center spip_document_center spip_document_avec_legende' data-legende-len=&#034;186&#034; data-legende-lenx=&#034;xxx&#034;
&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/jpg/solarpowerplantserpa.jpg' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/jpeg&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH375/solarpowerplantserpa-57e0d.jpg?1680688496' width='500' height='375' alt='' /&gt;&lt;/a&gt;
&lt;figcaption class='spip_doc_legende'&gt; &lt;div class='spip_doc_titre crayon document-titre-408 '&gt;&lt;strong&gt;Le silicium, pr&#233;sent dans le quartz, est un m&#233;tal utilis&#233; dans la fabrication des panneaux photovolta&#239;ques
&lt;/strong&gt;&lt;/div&gt; &lt;div class='spip_doc_credits crayon document-credits-408 '&gt;Ceinturion / Wikimedia Commons / CC BY-SA-3.0 / File:SolarPowerPlantSerpa.jpg
&lt;/div&gt;
&lt;/figcaption&gt;&lt;/figure&gt;
&lt;/div&gt;&lt;/div&gt;
		
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	</item>
<item xml:lang="en">
		<title>Tumulus</title>
		<link>https://expoos.mmx.bzh/article471.html</link>
		<guid isPermaLink="true">https://expoos.mmx.bzh/article471.html</guid>
		<dc:date>2022-07-07T20:15:14Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>en</dc:language>
		<dc:creator>amenez</dc:creator>



		<description>
&lt;p&gt;Stone : pink granite Type : plutonic magmatic rock Age : 300 millions years Quarry : la Clart&#233;, Perros-Guirrec (C&#244;tes d'Armor) &lt;br class='autobr' /&gt;
A Young One &lt;br class='autobr' /&gt;
This pink granite forms the outer part of the Ploumanac'h granite complex. It is part of the lineament of &#8220;red granites&#8221; of the Armorican Massif. These granites, about 300 million years old, are the youngest in Brittany. They stretch from the island of Ouessant in Finist&#232;re to Barfleur in the Manche department. &lt;br class='autobr' /&gt;
An Icon of Breton Geological Heritage (&#8230;)&lt;/p&gt;


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&lt;a href="https://expoos.mmx.bzh/rubrique39.html" rel="directory"&gt;Curious Breton garden&lt;/a&gt;


		</description>


 <content:encoded>&lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L150xH100/img_7979_niv-2-5c6d3.jpg?1680270100' class='spip_logo spip_logo_right' width='150' height='100' alt=&#034;&#034; /&gt;
		&lt;div class='rss_texte'&gt;&lt;blockquote class=&#034;spip&#034;&gt;
&lt;p&gt;
&lt;strong&gt;Stone&lt;/strong&gt; : pink granite&lt;br class='autobr' /&gt;
&lt;strong&gt;Type&lt;/strong&gt; : plutonic magmatic rock&lt;br class='autobr' /&gt;
&lt;strong&gt;Age&lt;/strong&gt; : 300 millions years&lt;br class='autobr' /&gt;
&lt;strong&gt;Quarry&lt;/strong&gt; : la Clart&#233;, Perros-Guirrec (C&#244;tes d'Armor)&lt;/p&gt;
&lt;/blockquote&gt;&lt;h2 class=&#034;spip&#034;&gt;A Young One&lt;/h2&gt;
&lt;p&gt;This pink granite forms the outer part of the Ploumanac'h granite complex. It is part of the lineament of &#8220;red granites&#8221; of the Armorican Massif. These granites, about 300 million years old, are the youngest in Brittany. They stretch from the island of Ouessant in Finist&#232;re to Barfleur in the Manche department.&lt;/p&gt;
&lt;div class='spip_document_403 spip_document spip_documents spip_document_image spip_documents_center spip_document_center spip_document_avec_legende' data-legende-len=&#034;63&#034; data-legende-lenx=&#034;x&#034;
&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/png/granites_rouges_sans_titre.png' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/png&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH500/granites_rouges_sans_titre-83b69.png?1680688497' width='500' height='500' alt='' /&gt;&lt;/a&gt;
&lt;figcaption class='spip_doc_legende'&gt; &lt;div class='spip_doc_titre crayon document-titre-403 '&gt;&lt;strong&gt;Les granites rouges sont les plus jeunes granites de Bretagne
&lt;/strong&gt;&lt;/div&gt; &lt;/figcaption&gt;&lt;/figure&gt;
&lt;/div&gt;&lt;h2 class=&#034;spip&#034;&gt;An Icon of Breton Geological Heritage&lt;/h2&gt;
&lt;p&gt;This granite is the origin of one of Brittany's main tourist attractions: the famous &#8220;Pink Granite Coast&#8221; in the C&#244;tes d'Armor department. These coastal landscapes, made up of massive pink granite boulders stacked in a wildly chaotic manner with improbable shapes, captivate visitors. Over 800,000 people visit the Ploumanac'h site each year.&lt;/p&gt;
&lt;div class='spip_document_404 spip_document spip_documents spip_document_image spip_documents_center spip_document_center spip_document_avec_legende' data-legende-len=&#034;185&#034; data-legende-lenx=&#034;xxx&#034;
&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/jpg/804-tregastel-tregastel-rocher-roi-gradlon.jpg' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/jpeg&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH313/804-tregastel-tregastel-rocher-roi-gradlon-19a92.jpg?1680688497' width='500' height='313' alt='' /&gt;&lt;/a&gt;
&lt;figcaption class='spip_doc_legende'&gt; &lt;div class='spip_doc_titre crayon document-titre-404 '&gt;&lt;strong&gt;Couronne du Roi Gradlon &#224; Tr&#233;gastel
&lt;/strong&gt;&lt;/div&gt; &lt;div class='spip_doc_credits crayon document-credits-404 '&gt;Archives d&#233;partementales des C&#244;tes d'Armor / Wikimedia Commons / Licence Ouverte 1.0 / File:Tr&#233;gastel - Rocher du roi Gradlon - AD22 - 16FI6270.jpg
&lt;/div&gt;
&lt;/figcaption&gt;&lt;/figure&gt;
&lt;/div&gt;&lt;h2 class=&#034;spip&#034;&gt;Why Is It Pink?&lt;/h2&gt;
&lt;p&gt;Clart&#233; granite is a coarse-grained granite, especially rich in large feldspar crystals (potassium feldspars) that range in color from pink to bright red. This coloration is due to the presence of small amounts of iron oxide impurities within these minerals. It also contains quartz and black mica.&lt;/p&gt;
&lt;div class='spip_document_405 spip_document spip_documents spip_document_image spip_documents_center spip_document_center'&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/jpg/img_8154_courbe.jpg' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/jpeg&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH333/img_8154_courbe-ed071.jpg?1680688497' width='500' height='333' alt='' /&gt;&lt;/a&gt;
&lt;/figure&gt;
&lt;/div&gt;&lt;h2 class=&#034;spip&#034;&gt;The &#8220;Rose de la Clart&#233;&#8221;&lt;/h2&gt;
&lt;p&gt;Its commercial name is Rose de la Clart&#233;. This granite is commonly used for memorials (e.g., the General de Gaulle memorial in Colombey-les-Deux-&#201;glises) and funerary furnishings. It is also used for flooring (like on rue de Siam in Brest), building facades (such as the European Court of Justice in Luxembourg), outdoor and indoor fixtures, furniture, and decorative elements.&lt;/p&gt;&lt;/div&gt;
		
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	</item>
<item xml:lang="en">
		<title>Labyrinth</title>
		<link>https://expoos.mmx.bzh/article469.html</link>
		<guid isPermaLink="true">https://expoos.mmx.bzh/article469.html</guid>
		<dc:date>2022-07-07T20:15:12Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>en</dc:language>
		<dc:creator>amenez</dc:creator>



		<description>
&lt;p&gt;Stone : mylonitic granite Type : metamorphic rock derived from a magmatic rock Age : 310 million years Quarry : Poulmarh, Grand Champ (Morbihan) &lt;br class='autobr' /&gt;
A Deeply Crushed Rock &lt;br class='autobr' /&gt;
The term &#8220;mylonite&#8221; refers to any rock that has been crushed to a finer or coarser degree (from the Ancient Greek &#8220;mul&#244;n&#8221;, meaning &#8220;mill&#8221;). The minerals within the rock retain signs of this deformation. The mylonite exposed at the Poulmarh quarry is a former granite &#8212; specifically, the Sainte-Anne d'Auray granite. This rock (&#8230;)&lt;/p&gt;


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		</description>


 <content:encoded>&lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L150xH100/img_8150_niv-2-737b3.jpg?1680270101' class='spip_logo spip_logo_right' width='150' height='100' alt=&#034;&#034; /&gt;
		&lt;div class='rss_texte'&gt;&lt;blockquote class=&#034;spip&#034;&gt;
&lt;p&gt;
&lt;strong&gt;Stone&lt;/strong&gt; : mylonitic granite&lt;br class='autobr' /&gt;
&lt;strong&gt;Type&lt;/strong&gt; : metamorphic rock derived from a magmatic rock&lt;br class='autobr' /&gt;
&lt;strong&gt;Age&lt;/strong&gt; : 310 million years&lt;br class='autobr' /&gt;
&lt;strong&gt;Quarry&lt;/strong&gt; : Poulmarh, Grand Champ (Morbihan)&lt;/p&gt;
&lt;/blockquote&gt;&lt;h2 class=&#034;spip&#034;&gt;A Deeply Crushed Rock&lt;/h2&gt;
&lt;p&gt;The term &#8220;mylonite&#8221; refers to any rock that has been crushed to a finer or coarser degree (from the Ancient Greek &#8220;mul&#244;n&#8221;, meaning &#8220;mill&#8221;). The minerals within the rock retain signs of this deformation. The mylonite exposed at the Poulmarh quarry is a former granite &#8212; specifically, the Sainte-Anne d'Auray granite. This rock was crushed more than 15 kilometers deep and marks the path of a major fault in Brittany: the South Armorican Shear Zone (see page 10). Other mylonites are found along this major tectonic feature.&lt;/p&gt;
&lt;h2 class=&#034;spip&#034;&gt;Perfect for Aggregate Production&lt;/h2&gt;
&lt;p&gt;This naturally crushed rock is ideally suited for producing aggregates. Aggregate refers to rock fragments smaller than 125 mm (including gravel, crushed stone, and sand). The Grand-Champ quarry, opened in the 1950s, now operates an ultra-modern processing plant &#8212; one of the largest in Europe &#8212; capable of producing over 6,000 tonnes of material per day, or about 2 million tonnes annually. It primarily supplies the local construction and public works markets.&lt;/p&gt;
&lt;h2 class=&#034;spip&#034;&gt;Caution: Nesting Area&lt;/h2&gt;
&lt;p&gt;The large sand piles stored in the quarry attract migratory swallows. They come to settle there during the summer breeding season, digging their nests into the artificial sand cliffs. Quarry operators, mindful of this beneficial coexistence, create special nesting mounds &#8212; about 4 to 5 meters high &#8212; so the birds can breed there peacefully.&lt;/p&gt;
&lt;div class='spip_document_400 spip_document spip_documents spip_document_image spip_documents_center spip_document_center spip_document_avec_legende' data-legende-len=&#034;104&#034; data-legende-lenx=&#034;xx&#034;
&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/jpg/20180517_155919.jpg' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/jpeg&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH281/20180517_155919-83229.jpg?1680688498' width='500' height='281' alt='' /&gt;&lt;/a&gt;
&lt;figcaption class='spip_doc_legende'&gt; &lt;div class='spip_doc_credits crayon document-credits-400 '&gt;Oiseaux en cours de nidification / Carri&#232;re de Grand-Champ / CMGO / Carri&#232;res et Mat&#233;riaux Grand-Ouest
&lt;/div&gt;
&lt;/figcaption&gt;&lt;/figure&gt;
&lt;/div&gt;&lt;h2 class=&#034;spip&#034;&gt;6.4 Tonnes of Aggregate per Person per Year&lt;/h2&gt;
&lt;p&gt;According to a report by the National Union of Aggregate Producers (UNPG), the average consumption of aggregates in France was 6.4 tonnes per inhabitant per year between 1978 and 2015. Each year, more than 400 million tonnes of aggregates supply the construction and public works sectors. Building a road or railway requires between 10,000 and 15,000 tonnes of aggregates per kilometer. A house requires between 100 and 300 tonnes, and a high school between 2,000 and 4,000 tonnes.&lt;/p&gt;
&lt;div class='spip_document_401 spip_document spip_documents spip_document_image spip_documents_center spip_document_center spip_document_avec_legende' data-legende-len=&#034;92&#034; data-legende-lenx=&#034;xx&#034;
&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/jpg/cmgo-13.jpg' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/jpeg&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH336/cmgo-13-c6aa1.jpg?1680688498' width='500' height='336' alt='' /&gt;&lt;/a&gt;
&lt;figcaption class='spip_doc_legende'&gt; &lt;div class='spip_doc_credits crayon document-credits-401 '&gt;Centrale &#224; granulats / Carri&#232;re de Grand-Champ / CMGO / Carri&#232;res et Mat&#233;riaux Grand-Ouest
&lt;/div&gt;
&lt;/figcaption&gt;&lt;/figure&gt;
&lt;/div&gt;&lt;/div&gt;
		
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	</item>
<item xml:lang="en">
		<title>Small bench</title>
		<link>https://expoos.mmx.bzh/article467.html</link>
		<guid isPermaLink="true">https://expoos.mmx.bzh/article467.html</guid>
		<dc:date>2022-07-07T20:15:10Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>en</dc:language>
		<dc:creator>amenez</dc:creator>



		<description>
&lt;p&gt;Stone : red sandstone Type : sedimentary rock Age : 480 million years Quarry : Lourtuais, Erquy (C&#244;tes d'Armor) &lt;br class='autobr' /&gt;
Multicolored Sand &lt;br class='autobr' /&gt;
Sandstone is a sedimentary rock formed from ancient hardened sand grains. The polished surface of the rock layer reveals horizons of different colors. These indicate variations in the composition of the sands. The darker layers are very rich in heavy minerals, such as iron or manganese oxides. Some of the lighter layers show cross-bedding; these features, (&#8230;)&lt;/p&gt;


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&lt;a href="https://expoos.mmx.bzh/rubrique39.html" rel="directory"&gt;Curious Breton garden&lt;/a&gt;


		</description>


 <content:encoded>&lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L150xH100/logo_petit_banc-2-8d0c7.jpg?1657266102' class='spip_logo spip_logo_right' width='150' height='100' alt=&#034;&#034; /&gt;
		&lt;div class='rss_texte'&gt;&lt;blockquote class=&#034;spip&#034;&gt;
&lt;p&gt;
&lt;strong&gt;Stone&lt;/strong&gt; : red sandstone&lt;br class='autobr' /&gt;
&lt;strong&gt;Type&lt;/strong&gt; : sedimentary rock&lt;br class='autobr' /&gt;
&lt;strong&gt;Age&lt;/strong&gt; : 480 million years&lt;br class='autobr' /&gt;
&lt;strong&gt;Quarry&lt;/strong&gt; : Lourtuais, Erquy (C&#244;tes d'Armor)&lt;/p&gt;
&lt;/blockquote&gt;&lt;h2 class=&#034;spip&#034;&gt;Multicolored Sand&lt;/h2&gt;
&lt;p&gt;Sandstone is a sedimentary rock formed from ancient hardened sand grains. The polished surface of the rock layer reveals horizons of different colors. These indicate variations in the composition of the sands. The darker layers are very rich in heavy minerals, such as iron or manganese oxides. Some of the lighter layers show cross-bedding; these features, well known to geologists, indicate a more turbulent depositional environment. The sands, transported by rivers with variable flow rates, were deposited on a piedmont plain at the base of hills.&lt;/p&gt;
&lt;div class='spip_document_398 spip_document spip_documents spip_document_image spip_documents_center spip_document_center'&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/png/formation_gres_erquy_cadrage.png' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/png&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH196/formation_gres_erquy_cadrage-5fc68.png?1680688498' width='500' height='196' alt='' /&gt;&lt;/a&gt;
&lt;/figure&gt;
&lt;/div&gt;&lt;h2 class=&#034;spip&#034;&gt;Millions of 10x10x10&lt;/h2&gt;
&lt;p&gt;The exploitation of the sandstones at Erquy began in the late 18th century and ended in the 1960s. The quarries mainly produced paving stones (10x10x10 cm) but also rubble stones, curb stones, and door and window lintels and frames. Quarry activity peaked between 1900 and 1930. Quarry waste was used in the construction of the Rance tidal power station dam in the early 1960s. All materials were exported by sea. Today, an interpretive trail allows visitors to discover the history of the quarry workers. The extraction site at Lourtuais is located 400 meters north of these former quarries.&lt;/p&gt;
&lt;div class='spip_document_397 spip_document spip_documents spip_document_image spip_documents_center spip_document_center spip_document_avec_legende' data-legende-len=&#034;243&#034; data-legende-lenx=&#034;xxx&#034;
&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH313/les_carrieres_industrielles_de_l_ouest__erquy__-_la_taille_des_pierres_et_la_voie_ferree_decauville_utilisee_avec_des_wagonnets_pour_le_transport-563a5.jpg?1680688498' width='500' height='313' alt='' /&gt;
&lt;figcaption class='spip_doc_legende'&gt; &lt;div class='spip_doc_credits crayon document-credits-397 '&gt;Archives d&#233;partementales des C&#244;tes d'Armor / Wikimedia Commons / Licence Ouverte 1.0 / File:Les carri&#232;res industrielles de l'Ouest (Erquy) - La taille des pierres et la voie ferr&#233;e Decauville utilis&#233;e avec des wagonnets pour le transport.jpg
&lt;/div&gt;
&lt;/figcaption&gt;&lt;/figure&gt;
&lt;/div&gt;&lt;h2 class=&#034;spip&#034;&gt;Opening, Expanding, Closing, Redeveloping&lt;/h2&gt;
&lt;p&gt;Opening or expanding a quarry is not something done on a whim. The company must prepare an authorization request and submit it to the prefecture services. This study details how the quarry will be operated and proposes solutions to manage its environmental impacts (water, noise, dust, biodiversity, landscape, etc.). It also outlines the site's rehabilitation plan after operations end. The company is required to restore the site. The maximum duration of operation is set at 30 years but is renewable.&lt;/p&gt;
&lt;div class='spip_document_396 spip_document spip_documents spip_document_image spip_documents_center spip_document_center spip_document_avec_legende' data-legende-len=&#034;34&#034; data-legende-lenx=&#034;x&#034;
&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/jpg/img_8321_mod_erquy.jpg' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/jpeg&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH333/img_8321_mod_erquy-b52e0.jpg?1680688498' width='500' height='333' alt='' /&gt;&lt;/a&gt;
&lt;figcaption class='spip_doc_legende'&gt; &lt;div class='spip_doc_titre crayon document-titre-396 '&gt;&lt;strong&gt;Ancienne carri&#232;re des lacs bleus
&lt;/strong&gt;&lt;/div&gt; &lt;/figcaption&gt;&lt;/figure&gt;
&lt;/div&gt;&lt;/div&gt;
		
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	</item>
<item xml:lang="en">
		<title>Large bench</title>
		<link>https://expoos.mmx.bzh/article465.html</link>
		<guid isPermaLink="true">https://expoos.mmx.bzh/article465.html</guid>
		<dc:date>2022-07-07T20:15:09Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>en</dc:language>
		<dc:creator>amenez</dc:creator>



		<description>
&lt;p&gt;Stone : siltite (almost transformed into a slate) Type : metamorphic rock derived from a sedimentary rock Age : between 590 and 540 million years Carri&#232;re : Ripennelais, Saint-Aubin des Landes (Ille-et-Vilaine) &lt;br class='autobr' /&gt;
Rustic Slates &lt;br class='autobr' /&gt;
This rock has been exploited for over two centuries, initially used to make lauzes, those rustic, thick slates used on roofs in certain regions of France. However, due to its poor slate quality, this rock&#8212;over 500 million years old&#8212;was no longer in demand, and slate (&#8230;)&lt;/p&gt;


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		</description>


 <content:encoded>&lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L150xH100/img_8221_mod_banc-2-633fd.jpg?1680270101' class='spip_logo spip_logo_right' width='150' height='100' alt=&#034;&#034; /&gt;
		&lt;div class='rss_texte'&gt;&lt;blockquote class=&#034;spip&#034;&gt;
&lt;p&gt;
&lt;strong&gt;Stone&lt;/strong&gt; : siltite (almost transformed into a slate)&lt;br class='autobr' /&gt;
&lt;strong&gt;Type&lt;/strong&gt; : metamorphic rock derived from a sedimentary rock&lt;br class='autobr' /&gt;
&lt;strong&gt;Age&lt;/strong&gt; : between 590 and 540 million years&lt;br class='autobr' /&gt;
&lt;strong&gt;Carri&#232;re&lt;/strong&gt; : Ripennelais, Saint-Aubin des Landes (Ille-et-Vilaine)&lt;/p&gt;
&lt;/blockquote&gt;&lt;h2 class=&#034;spip&#034;&gt;Rustic Slates&lt;/h2&gt;
&lt;p&gt;This rock has been exploited for over two centuries, initially used to make lauzes, those rustic, thick slates used on roofs in certain regions of France. However, due to its poor slate quality, this rock&#8212;over 500 million years old&#8212;was no longer in demand, and slate production had to be abandoned by the end of the 1990s.&lt;/p&gt;
&lt;div class='spip_document_392 spip_document spip_documents spip_document_image spip_documents_center spip_document_center'&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/jpg/img_8186_niv.jpg' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/jpeg&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH333/img_8186_niv-3b86e.jpg?1680688499' width='500' height='333' alt='' /&gt;&lt;/a&gt;
&lt;/figure&gt;
&lt;/div&gt;&lt;h2 class=&#034;spip&#034;&gt;A Friend Against the Rain&lt;/h2&gt;
&lt;p&gt;Since it was easier to crush the material into small pieces than to extract slates, by the 1960s, the company diversified its production and specialized in producing flakes to utilize quarry waste. These flakes were then used in the manufacture of bituminous shingles (shingle in English). They protect tar from solar and lunar radiation and remain effective allies for rain protection.&lt;/p&gt;
&lt;div class='spip_document_393 spip_document spip_documents spip_document_image spip_documents_center spip_document_center spip_document_avec_legende' data-legende-len=&#034;81&#034; data-legende-lenx=&#034;xx&#034;
&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/jpg/shingle_roof_2_2017-06-14.jpg' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/jpeg&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH375/shingle_roof_2_2017-06-14-c4c9e.jpg?1680688499' width='500' height='375' alt='' /&gt;&lt;/a&gt;
&lt;figcaption class='spip_doc_legende'&gt; &lt;div class='spip_doc_credits crayon document-credits-393 '&gt;FASTILY / Wikimedia Commons / CC BY-SA-4.0 / File:Shingle roof 2 2017-06-14.jpg
&lt;/div&gt;
&lt;/figcaption&gt;&lt;/figure&gt;
&lt;/div&gt;&lt;h2 class=&#034;spip&#034;&gt;The Age of Mulching&lt;/h2&gt;
&lt;p&gt;In the 2000s, the family company ventured into &#034;mineral mulching&#034; for the landscaping sector. This mulch, complementary to plant-based mulching, has numerous advantages: it retains soil heat, provides shelter for wildlife, remains permeable to water and air, and helps limit weed growth.&lt;/p&gt;
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&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;a href='https://expoos.mmx.bzh/IMG/jpg/img_8314_mod.jpg' class=&#034;spip_doc_lien mediabox&#034; type=&#034;image/jpeg&#034;&gt; &lt;img src='https://expoos.mmx.bzh/local/cache-vignettes/L500xH750/img_8314_mod-e2c9d.jpg?1680688500' width='500' height='750' alt='' /&gt;&lt;/a&gt;
&lt;/figure&gt;
&lt;/div&gt;&lt;h2 class=&#034;spip&#034;&gt;Made with&#8230; Brilliance&lt;/h2&gt;
&lt;p&gt;This siltstone belongs to a geological formation dated to the Briov&#233;rien period, a geological time frame between 670 and 540 million years ago. The term &#034;Briov&#233;rien&#034; comes from the Latin briovera, meaning &#034;bridge over the Vire,&#034; which is the former name of the town of Saint-L&#244; in Normandy, where this geological formation also outcrops.&lt;/p&gt;&lt;/div&gt;
		
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