{"id":15305,"date":"2025-05-20T10:46:53","date_gmt":"2025-05-20T08:46:53","guid":{"rendered":"https:\/\/selfguided-toscana.it\/poi\/the-giants-pots-en\/"},"modified":"2025-05-20T10:46:53","modified_gmt":"2025-05-20T08:46:53","slug":"the-giants-pots-en","status":"publish","type":"poi","link":"https:\/\/selfguided-toscana.it\/en\/poi\/the-giants-pots-en\/","title":{"rendered":"The giants&#8217; pots"},"content":{"rendered":"\t<section class=\"l-section wpb_row height_small with_img with_overlay wm_header_section\">\n\t\t<div class=\"l-section-img loaded wm-header-image\" style=\"background-image: url(https:\/\/ecmedia.s3.eu-central-1.amazonaws.com\/EcMedia\/76424.jpg);background-repeat: no-repeat;\">\n\t\t<\/div>\n\t\t<div class=\"l-section-h i-cf wm_header_wrapper\">\n\t\t<\/div>\n\t<\/section>\n\n\t<div class=\"wm_body_section\">\n\t\t\t\t\t<h1 class=\"align_left wm_header_title\">\n\t\t\t\tThe giants' pots\t\t\t<\/h1>\n\t\t\t\t\t\t\t\t<div class=\"wm_activities wm_container>\n\t\t\t\t\t\t\t\t\t\t\t<span class=\"wm_activity\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"wm_activity_icon\"><svg xmlns='http:\/\/www.w3.org\/2000\/svg' viewBox='0 0 1024 1024' width='32' height='32'><circle fill=\"darkorange\"  cx='512' cy='512' r='512'\/><g fill=\"white\" transform='scale(0.8 0.8) translate(100, 100)'><path d='M1000.928 451.648l-145.536-145.472-43.008-43.296-102.4-102.4c-3.776-4.256-9.248-6.944-15.36-6.944-4.992 0-9.6 1.792-13.152 4.768l0.032-0.032-0.736 0.608-64.928 64.992c-3.552 3.552-5.728 8.448-5.728 13.856s2.208 10.304 5.728 13.856v0l98.304 97.568c3.872 7.584 6.144 16.576 6.144 26.048 0 4.224-0.448 8.32-1.28 12.288l0.064-0.384-24.448 24.512-121.92 121.792c-3.552-3.552-8.448-5.728-13.856-5.728s-10.304 2.208-13.856 5.728v0l-62.944 57.408-216.672-216.736c-0.8-3.232-1.248-6.944-1.248-10.752 0-8.832 2.432-17.088 6.688-24.128l-0.128 0.224c19.424-35.104 43.904-64.864 72.864-89.536l0.448-0.384c65.6-64.864 125.6-106.144 127.040-110.944s-44.448-4.512-128.416 45.056c-52.16 30.848-97.248 65.696-137.6 105.376l0.096-0.096h-0.352l-199.136 199.264c-3.456 2.976-5.664 7.392-5.664 12.288 0 4.032 1.472 7.712 3.904 10.528l-0.032-0.032 0.48 0.544 37.6 37.6c2.848 2.816 6.752 4.544 11.072 4.544s8.224-1.728 11.072-4.544v0l126.368-126.912c6.080-3.104 13.28-4.928 20.896-4.928 3.36 0 6.624 0.352 9.792 1.024l-0.32-0.064 214.976 214.848-209.024 191.136c-3.424 3.52-5.536 8.352-5.536 13.664s2.112 10.144 5.536 13.664v0l82.944 82.944c3.52 3.424 8.352 5.504 13.664 5.504s10.112-2.112 13.664-5.504v0l177.888-194.848 178.912 195.936c2.848 2.848 6.752 4.608 11.104 4.608s8.256-1.76 11.104-4.608l66.432-66.432c2.784-2.848 4.512-6.72 4.512-11.040s-1.728-8.192-4.512-11.040v0l-199.072-181.856 44.64-48.8c3.552-3.552 5.728-8.448 5.728-13.856s-2.208-10.304-5.728-13.856v0l146.144-146.016c3.552-0.768 7.648-1.216 11.808-1.216 9.504 0 18.464 2.272 26.4 6.272l-0.32-0.16 97.76 98.496c3.52 3.552 8.416 5.728 13.824 5.728s10.304-2.208 13.824-5.728v0l64.992-64.928 0.608-0.736c3.040-3.552 4.928-8.224 4.928-13.312 0-6.176-2.752-11.712-7.072-15.488l-0.032-0.032z'\/><\/g><\/svg><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"wm_activity_name\">N\/A<\/span>\n\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t<span class=\"wm_activity\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"wm_activity_icon\"><svg xmlns='http:\/\/www.w3.org\/2000\/svg' viewBox='0 0 1024 1024' width='32' height='32'><circle fill=\"darkorange\"  cx='512' cy='512' r='512'\/><g fill=\"white\" transform='scale(0.8 0.8) translate(100, 100)'><path d='M410.965 575.147c-11.924 8.744-22.25 18.637-31.156 29.72l-0.247 0.317-310.613-238.933c30.028-39.132 63.95-73.054 101.791-102.129l1.292-0.953zM851.968 263.851l-238.933 310.613c11.655 8.957 21.763 19.065 30.436 30.335l0.284 0.385 311.296-238.933c-30.015-38.886-63.936-72.59-101.762-101.434l-1.321-0.966zM498.633 683.547c-50.513 6.837-89.038 49.682-89.038 101.524 0 56.554 45.846 102.4 102.4 102.4s102.4-45.846 102.4-102.4c0-4.712-0.318-9.351-0.935-13.894l0.059 0.529c-6.839-50.511-49.683-89.035-101.524-89.035-4.711 0-9.348 0.318-13.891 0.934l0.529-0.059zM438.955 152.576c-52.297 6.768-99.755 19.946-144.166 38.888l3.537-1.341 150.187 363.179c12.126-5.671 26.196-9.761 40.977-11.54l0.666-0.065zM585.045 153.259l-51.2 388.437c15.512 2.061 29.561 5.89 42.773 11.335l-1.13-0.413 150.187-361.813c-40.986-18.289-88.524-31.525-138.331-37.329l-2.298-0.218z'\/><\/g><\/svg><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"wm_activity_name\">Panoramic point<\/span>\n\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<div class=\"wm_container\">\n\t\t\t<div class=\"wm_left_wrapper\">\n\t\t\t\t<iframe class=\"wm_iframe_map\" src=\"https:\/\/geohub.webmapp.it\/poi\/simple\/43157?locale=en\" loading=\"lazy\"><\/iframe>\n\t\t\t\t\t\t\t\t\t<div class=\"wm_body_description_content\">\n\t\t\t\t\t\t<p>Access to the ditch Anguillaja: parked the vehicle on the edge of the provincial road of Val d\u2019Arni (687 m above sea level), which leads to Castelnuovo Garfagnana, you walk on foot along an old cart track, which opens on the left and descends towards the Dry T\u00f9rrite. After 250 m you reach the watercourse which, as a rule, is completely dry, since it is characterized by a subalveous circulation. After having traveled the arid bottom in a northerly direction, while the river shaft draws a recessed meander, you immediately meet the confluence from the left of the Anguillaja ditch (650 m above sea level), largely modified by the old cuts and the abandoned residues of a Marble quarry. The mining activity also canceled the first \u2018potholes\u2019 that existed in the lower part of the same ditch, artificially shaping its bottom and its side walls.<br \/>\nThe Anguillaja is an intermittent watercourse on a temporary basis, on the occasion of heavy rains, which presents some remarkable \u2018potholes\u2019, described for the first time by Masini (1929). At that time, the last 300 m of the ditch descending from M. Sumbra, showed 13 large cauldron cavities. Their number then decreased due to the destruction produced years ago by the disused quarry of its lower section. The surviving \u2018potholes\u2019, now protected by the Regional Park, are easily observable by continuing the short itinerary along the Anguillaja. The ascent of the ditch is relatively easy at the beginning and, the first morphological jump, is overcome thanks to a small iron staircase. This leads to the spectacular succession of three \u2018potholes\u2019 of significant proportions, completely carved out of marble (see photo on the side).<br \/>\nFurther on, the route requires practice in the use of the double rope and in climbing adherence on rock.<\/p>\n<p>Morphogenesis: the \u2018pots of the giants\u2019 often owe their origin to the abrasive action of rotating pebbles. The development requires several coincident conditions, including the swirling movement of the river current and a coherent and homogeneous rocky substrate, such as the marble of M. Sumbra.<br \/>\nThe \u2018mufflers\u2019 of Anguillaja and Fatonero also seem to refer to this model, as the signs of mechanical erosion on the inner edges of the large cauldron cavity shown on the side would demonstrate.<br \/>\nHowever, some Authors have hypothesized a genesis of these \u2018potholes\u2019 in a forced regime, through subglacial tunnels that were to be located in the southern slope of Sumbra and Fiocca, in correspondence with glaciers or perennial snowfields formed during the last ice age.<br \/>\nFor others, chemical dissolution (surface karst) may have initially prepared the cavities, on which the hydrodynamic action then had a prevalent or exclusive reason (Federici et alii, 1981).<\/p>\n<p>A look at the Fatonero ditch, the Fiocca and the Sumbra<br \/>\nFrom the provincial road of Val d\u2019Arni, 700 m further upstream from the Anguillaja, the Fatonero ditch is easily identifiable, of which the last 400-500 m of stretch can be observed, descending from M. Fiocca. The \u2018potholes\u2019 have been numbered decreasing as the ditch goes up: in all they are 21 and the same size as the twin ditch. They too are carved out of marble.<br \/>\nOn the way up the M. Fiocca, from the Fatonero ditch, we find, in succession, Marbles, Selciferous Limestones, Diaspri, Selciferous Limestones at Entrochi, Sericitic Schists and Pseudomacigno, with different repetitions due to minor folds. It should also be noted the presence of three tiny klippe of cavernous limestone. M. Sumbra, on the other hand, consists mainly of Marbles and Selciferous Limestones. The southern slopes of these two hills are characterized above all by karst and glacial modeling. The rounded furrows of the south wall of the Sumbra are linked to cryonal processes, due to perennial snowfields or small ephemeral masses of ice.<\/p>\n\t\t\t\t\t<\/div>\n\t\t\t\t\t\t\t<\/div>\n\n\t\t\t<div class=\"wm_right_wrapper\">\n\t\t\t\t<div class=\"wm_body_gallery\">\n\t\t\t\t\t\t\t\t\t\t\t<div class=\"swiper-container\">\n\t\t\t\t\t\t\t<div class=\"swiper-wrapper\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<div class=\"swiper-slide\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"https:\/\/ecmedia.s3.eu-central-1.amazonaws.com\/EcMedia\/76424.jpg\" data-lightbox=\"track-gallery\" data-title=\"\">\n\t\t\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" src=\"https:\/\/ecmedia.s3.eu-central-1.amazonaws.com\/EcMedia\/Resize\/400x200\/76424_400x200.jpg\" alt=\"\" loading=\"lazy\">\n\t\t\t\t\t\t\t\t\t\t\t<\/a>\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<div class=\"swiper-slide\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"https:\/\/ecmedia.s3.eu-central-1.amazonaws.com\/EcMedia\/76423.jpg\" data-lightbox=\"track-gallery\" data-title=\"\">\n\t\t\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" src=\"https:\/\/ecmedia.s3.eu-central-1.amazonaws.com\/EcMedia\/76423.jpg\" alt=\"\" loading=\"lazy\">\n\t\t\t\t\t\t\t\t\t\t\t<\/a>\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t\t\t<div class=\"swiper-pagination\"><\/div>\n\t\t\t\t\t\t\t<div class=\"swiper-button-prev\"><\/div>\n\t\t\t\t\t\t\t<div class=\"swiper-button-next\"><\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<div class=\"wm_info\">\n\t\t\t\t\t<div class=\"wm_info_item\"><span class=\"wm_related_urls\"> <span class=\"fa fa-external-link-alt\"><\/span> <a href=\"http:\/\/www.apuanegeopark.it\/apuanegeopark_geotur_marmitte.html\" target=\"_blank\">www.apuanegeopark.it<\/a><\/span><\/div>\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t<\/div>\n\t<\/div>\n\n\n\n\n\n\n\t<\/div>\n\n\t<script>\n\t\tdocument.addEventListener('DOMContentLoaded', function() {\n\t\t\tvar swiper = new Swiper('.swiper-container', {\n\t\t\t\tslidesPerView: 1,\n\t\t\t\tspaceBetween: 10,\n\t\t\t\tfreeMode: true,\n\t\t\t\tloop: true,\n\t\t\t\tpagination: {\n\t\t\t\t\tel: '.swiper-pagination',\n\t\t\t\t\tclickable: true,\n\t\t\t\t},\n\t\t\t\tnavigation: {\n\t\t\t\t\tnextEl: '.swiper-button-next',\n\t\t\t\t\tprevEl: '.swiper-button-prev',\n\t\t\t\t},\n\t\t\t});\n\t\t});\n\t<\/script>\n\n\n","protected":false},"featured_media":0,"template":"","meta":{"_acf_changed":false},"class_list":["post-15305","poi","type-poi","status-publish","hentry"],"acf":{"geohub_poi_id":"43157"},"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.3 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>The giants&#039; 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