#: locale=es ## Hotspot ### Texto HotspotPanoramaOverlayTextImage_18BE55EE_060C_E23E_4166_F72D41F51CB2.text = Northern quartzite alignment in which it is possible to verify \ the absence of glacial erosion forms, despite being above \ two thousand metres altitude of glacial erosion forms. HotspotPanoramaOverlayTextImage_1815825C_060C_E618_4184_5745548AC05E.text = Patch of slope regularised by \ laminar solifluction HotspotPanoramaOverlayTextImage_19584E21_0614_A1DC_4179_25237FE55B4A.text = Secondary calcalreous ridges in the shale furrow of the San Isidro \ Mountain Pass HotspotPanoramaOverlayTextImage_1B947C52_061C_E271_4187_BF58899DAB2C.text = Shale furrow of San Isidro \ Mountain Pass HotspotPanoramaOverlayTextImage_1801130F_0614_67DA_415F_518ACF614D5F.text = Toneo peak \ (2,091 m.) HotspotPanoramaOverlayTextImage_1951D497_061B_A2FB_4192_C656807AC09B.text = Torres peak \ (2,091 m.) ### Tooltip HotspotPanoramaOverlayArea_26EC0ED8_06F4_9E11_4182_49B4905AD646.toolTip = Fonfría peatbog occupying the interior of a glacial overdeepening basin. This peatbog is one of the most important \ on the southern slope of the Cantabrian Mountains, both for its age (more than 10,000 years old) \ and its thickness (generally more than 10 metres, although it can occasionally reach 30 metres). ## Media ### Imágen imlevel_26CE089E_06F4_620F_4194_6ABAB427B457.url = media/panorama_1BF51E49_0615_BE46_4184_65D88188F8C5_HS_15jdes3r_es.png imlevel_26D32952_06F4_6217_417C_2C8B90237420.url = media/panorama_1BF51E49_0615_BE46_4184_65D88188F8C5_HS_3uyn832w_es.png imlevel_26C0F691_06F4_6E15_4167_E39C204B18FD.url = media/panorama_1BF51E49_0615_BE46_4184_65D88188F8C5_HS_9hbu57sm_es.png imlevel_26CA0826_06F4_623C_4183_C966F0D9D4BE.url = media/panorama_1BF51E49_0615_BE46_4184_65D88188F8C5_HS_dxq9y87u_es.png imlevel_26C587E0_06F4_6E33_4198_B30D5B62D7DC.url = media/panorama_1BF51E49_0615_BE46_4184_65D88188F8C5_HS_qkimtc1j_es.png imlevel_26C64720_06F4_6E34_4192_2A8288F1C6A8.url = media/panorama_1BF51E49_0615_BE46_4184_65D88188F8C5_HS_u0ob6luw_es.png ### Título panorama_1BF51E49_0615_BE46_4184_65D88188F8C5.label = Fig_19 ## Tour ### Descripción ### Título tour.name = Fig_19 ## Ventana ### Cuerpo htmlText_18D6230A_06F4_A7F1_4183_4A64B9E62363.html =

Fonfría peatbog occupying the interior of a glacial overdeepening basin. This peatbog is one of the most important on the southern slope of the Cantabrian Mountains, both for its age (more than 10,000 years old) and its thickness (generally more than 10 metres, although it can occasionally reach 30 metres).