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And there was no way I could tell my mom what was going on. In the end, I got an appointment with a gynecologist and I found out it was stress. Three of my friends are still virgins. It lack of sexual activity, ed. That means that I get a turn, too. Dashed lines indicate moraines, solid lines mark the glacial thresholds, double dashed lines delineate protalus ramparts. The middle and lower sector of the Lotru valley is heavily forested, thus the glacial deposits are very difficult to identify.

Unfortunately, ground truthing of most of the published glacial record at lower altitudes has been impossible after the building of a major storage reservoir at Vidra. The scatter of exposure ages confirms the mixed origin of this We tentatively assigned a deglaciation age consistent with the rest of the ages produced from samples located in front of the Iezer Lake see above.

Pre-exposure on a rock cliff and transport on top of ice surface are likely the causes for the inheritance of nuclides in this boulder, here considered an outlier.

The last five samples produced from the moraines in this cirque come from a widespread moraine complex and it is unlikely to have been covered. All boulders were well embedded into the surface and unlikely to have suffered any modifications since their deposition.

They were subsequently filled with glacial sediments which stand as evidence of a reshaped and very diverse landscape. Previous studies in the Parang Mountains identified repeated glaciers advances and recessions during the last Quaternary glaciations In this part we present our interpretation of field evidence and the deglaciation chronology obtained with the surface exposure dating of moraine boulders.

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No suitable sites for cosmogenic nuclide surface exposure dating were found here. During the Late Glacial, the downwasting of ice in the upper valleys and cirques of the Parang Mountains Figs. These boulders are part of a deposit likely formed by the glacier flowing down from the North Mohoru cirque Figs. At roughly the same time, ice in the Iezer valley had already withdrawn towards the higher ground.

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In the Zanoaga Pietroasa cirque, this southward retreat of glacier caused the deposition of the moraine that blocked Fig. Probability density plots for the exposure ages obtained from glacial landforms. The ages are given with their analytical uncertainty. A faster retreat of ice occurred from the Lotru valley towards the Zaanoaga Mare cirque. Ice in this wide and shallow cirque would have received more solar radiation than the others cirques, speeding up the glacier retreat after separation from the Gaalcescu glacier.

The subsequent thinning and narrowing of ice towards the middle of the cirque is indicated by the erosional paths of two former ice flow that are still visible today around the large whaleback located on the glacial threshold Figs. One of the ice flows followed the main Zaanoaga stream on the north side while the secondary flow was probably joined to the Gaalcescu glacier. Although the Gaalcescu cirque had a smaller accumulation area, snow drift from the upper surfaces would have contributed to a thicker glacier Gellatly et al.

Also sheltered by steep high walls, the Galcescu ice retreated slower than the glacier in the Zaanoaga Mare cirque located at similar altitudes. The glacier located in the Caaldarea Dracului cirque was probably feeding the glacier that occupied the Gaalcescu cirque.

Following more retreat, the glacier in the Zaanoaga Mare cirque deposited the recessional moraines near the southern headwall Figs. The higher western compartment of the Zaanoaga Mare cirque likely preserved ice for longer times, similar to the Caaldarea Dracului cirque. Although evidence of glaciation exists in the middle and lower Lotru valley, no boulders or bedrock areas were found suitable for surface exposure dating of the maximum ice extent in the Paraang Mountains.

Moreover, based on the current morphological characters of the study area, it was not possible to establish whether a climatically controlled readvance occurred during the Late Glacial or the Younger Dryas, or whether the deglaciation occurred as a continuous event since the maximum ice extent. The retreat of ice towards the higher valleys and cirques in the Parang Mountains during the Late Glacial period is indicated by the exposure ages obtained from moraine boulders.

Braun et al. This is in good agreement with the warm and dry climate found at lower altitudes in north-western Romania Wohlfarth et al. Only weak cooling was observed in chironomid reconstruction during the Younger Dryas episode Toth et al. Glacial retreat compared to other records in Europe Similar climatic changes occurred in the mountains of Europe during the Late Glacial period. The last major The Younger Dryas cirque glaciers at high elevations in the Eastern Alps retreated at ca.

Conclusions Comparison of our reported ages to other chronologies within the region supports an interpretation that our data are accurate within the context of the study location, the outlined glacial stratigraphy, and within the context of latest Pleistocene climate change. The results presented in this study are consistent with cosmogenic nuclide exposure ages previously reported from adjacent areas.

Being located further away from the North Atlantic, a different climatic signal is more likely expected. Clima Romaniei. In: Bucuresti Bercia, Geological Map of Romania. Andric, Late quaternary vegetation and hydrological change at Ljubljansko barje Slovenia. Balco, Ballantyne,