Back to top Print this page. On the southern side we find: Precipitation intensity is colour coded, ranging from light blue to heavy purple. Lightning data provided by nowcast. Drizzle or light snow fall might be invisible for the radar. Cerbului Lake , Bratila Lake.
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Precipitation is estimated from radar and satellites. Test our new website. Satellite cloud cover past 2 hours.
High clouds and clouds with vertical development are displayed in white, low clouds and fog in grey. Click on the full-screen button to get a bigger view with more options. Fagaras Mountains are composed of metamorphic hard rocks, foundation, belonging crystalline schists, whose sistuozitate is very impotant in mountaineering. The valleys of Suru and Berivoiu are broad and deep U-shaped glaciers, the one sides and the other of the main ridge. On the transversal plan, from mountains to the plain Olt Country slope descends over m in less than 10km, horizontally.
North edges are short, strongly sloping and are loosing into Tara Olt plain and southern edges go down into the groove of Loviste depression. This map uses infrared satellite telemetry to calculate the temperature of the clouds. On the southern side we find: Fagaras Mountains are in the Meridional Carpathians, toward E-V, with a length of 70 km, width 40 km, stretching over an area of square kilometers, representing the most powerful massive alpine of Romania mountains.
Are found in the hollows and glacial valleys, offering tourists places with wonderful landscapes to halt. Cerbului LakeBratila Lake. The reliability of this forecast is medium. Location Fagaras Mountains are in the Meridional Carpathians, toward E-V, with a length of 70 km, width 40 km, stretching over an area of square kilometers, representing the most powerful massive alpine of Romania mountains.
Between November 1, – July 1,Transfagarasan road is closed.
Welcome to the website of the Fagaras Mountains, where you can mubtii updated information about Balea Cablecarview live images from Balea Lac, you can inform of the hiking trails munii the area, view maps and get acquainted with chalets and rates their updated.
This animation shows the cloud cover as observed by satellite. At night precipitation estimates from satellites are less accurate than during daytime. Back to top Print this page. Low clouds and fog are difficult to distinguish from ground temperatures and might therefore be inaccurate.
Here we meet peaks with elevations above – m such as Peak. On the ridge of Fagaras find: In sharp contrast to the glacial relief, the river and torrential appears, where the valley narrows suddenly are all less rocky slopes and sharp ridges disappear, relief continuing with large pastures and woods. Precipitation intensity is colour coded, ranging from light blue to heavy purple.
The first 4 time steps also show precipitation. We respect your privacy. In terms of longitudinal Fagaras Mountains looks like a huge stone wall that descends to the extremities, below m altitude. NEMS4 Last model run: Transylvanian slope consists of epizon shale, the weakly metamorphosed rocks formed at m depththe main ridge of crystalline schists of mezozona formed in to 14, m deep on the back and steep outcrops of shale with small white, black mica gneiss.
Fagaras Mountains are composed of a lot of crags and aligned peakswhich descends to the extremities below m, to Olt Valley and Dambovita’s depression.
For example Big Corner of Vistea and is m in altitude and Vistisoara is down to m. Different altitude layers can be selected in the top-right menu. Wind streamlines are animated on top of a wind speed or temperature map.
Drizzle or light snow fall might be invisible for the radar. Relief Fagaras Mountains tagaras composed of a lot of crags and aligned peakswhich descends to the extremities below m, to Olt Valley and Dambovita’s depression.