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View all photos Travellers' Choice. Read more. Property amenities. Paid public parking nearby. Breakfast buffet. Highchairs available.
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Meeting rooms. Baggage storage. Non-smoking hotel. Blackout curtains. Soundproof rooms. Air conditioning. Bottled water. Flatscreen TV. Clothes rack. Private bathrooms. Electric kettle.
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Complimentary toiletries. Hair dryer. Non-smoking rooms. Languages Spoken. Bierset Airport 6 mi See all flights. Maastricht-Aachen Airport 20 mi See all flights.
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Car Hire See all Liege car hire. Une Gaufrette Saperlipopette - La petite boutique. Write a review. Traveller rating. Selected filters. All reviews small boutique hotel old building high tech breakfast room great shower family room comfortable bed alley reception housekeeping parking minibar hallway. Mimi-RC wrote a review Jan Interesting, with potential. Quiet, on an old historic alley-like street between Place du Marche and the Meuse.
Interesting street Neuvice to walk through during the day but a bit creepy on a weeknight, and no one at the front desk after 9PM with minimal personnel on site during the day. Public rooms and breakfast room are beautifully renovated in this very old building.
Inner courtyard provides quietude and light, but we visited during winter. Buffet breakfast was fine but we prefer a la carte or traditional smaller breakfast Date of stay: January Service.
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Become a member. A marketplace you can trust We connect you with the best professionally managed properties and our marketing leading customer services can help you every step of the way. These results offer interesting perspectives for the investigation of the loess sequence related to archaeological applications. Geologists, geomorphologists and soil scientists usually consider this material as a sedimentary sequence with heterogeneities even at local scale palaeosols, unconformity surfaces, palaeovalleys In addition to preliminary survey works, characterization of loess and resulting interpretations are classically performed by sedimentological e.
Antoine et al. Ding et al. Smykatz-Kloss et al. Buylaert et al. Results of these studies point out a succession of layers and horizons including removed sediments, eventual tephra e. Pouclet et al. Moreover, loess deposits are very easily erodible, raising the complexity for stratigraphic studies due to the presence of locally eroded layers and unconformity surfaces.
These sections are unfortunately rare, often temporary and not deep enough. An alternative could be sampling from drillings but it becomes expensive for thick loess layers. Moreover, the recognition of horizons based on samples is not always easy. Indeed CPT is a common and worldwide test usually performed for civil engineering applications e.
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It is fast, repeatable, and economical, compared to drilling. CPT consists of pushing a cone tip at the end of a series of rods into the ground at constant rate to measure continuously or intermittently the resistance to penetration of the tip. Measurements of the friction resistance on the outer surface of tubes or on a surface sleeve can also be performed. Geotechnicians use CPTs to mechanically characterize subsoil layers in order to provide quantitative data on the mechanical behaviour through depth.
But civil engineering applications usually do not focus on a detailed loess stratigraphy study.
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Geotechnicians usually consider this material as a homogeneous fine soft material. Numerous studies also perform CPTs to distinguish between soil materials for environmental and agricultural applications e.
These applications rarely investigate a depth exceeding two metres beneath the ground surface. In this study the mechanical approach from CPT data is applied to Middle and Late Pleistocene loess located in the eastern part of the Hesbaye region. The region has no officially defined borders. It is, however, well-established to place the southern and eastern boundaries of the region at the top of the flank of the Meuse valley Fig.
The western limit is approximately a N-S axis extending from the Meuse valley to the city of Tienen. Location map of the places and regions mentioned in this paper. The dotted area represents the extent of the Hesbaye region.
Maastrichtian deposits are mainly composed of grey and white chalk containing continuous flint nodule layers — the Gulpen Formation Robaszynski, In the eastern part of the Hesbaye region, the Maastricht Formation composed of calcarenite is on top of the Gulpen Formation Robaszynski, A marine regression at the end of Maastrichtian caused erosion and dissolution of the top of the chalk and calcarenite layers, and resulted in a flint nodule conglomerate at the top of the Gulpen Formation. The sea covered again the eastern part of the Hesbaye during Selandian and Thanetian Paleocene.
During Rupelian early Oligocene new deposits covered the eastern part of the Hesbaye region. They are related to a marine transgression and are composed of fine sands, silts and clays of the Sint-Huibrechts-Hern Formation Laga, Evidence of Oligocene deposits has also been found at m a. At the end of Oligocene the sea receded for the last time. Finally the Oligocene deposits have been overlaid by aeolian silt layers during Quaternary. These deposits are mainly related to the last glaciation Weichselian. Due to the evidence of Oligocene marine sands at Baraque Michel, it has been estimated that the Ardenne massif has uplifted at least m in its NE part since Oligocene Demoulin, This inclination is related to the uplift of the Ardenne massif.
The main studied Middle and Late Pleistocene loess sequences in Middle Belgium are shown in Figure 1 see cross symbol. Upper part of Middle Pleistocene and lower part of Late Pleistocene loess sequences correlation in Middle Belgium modified, after Haesaerts et al. Haesaerts; infographic by E. Symbols legend: 1. B2t horizon leached horizon ; 7.