Prices are the average nightly price provided by our partners and may not include all taxes and fees. Taxes and fees that are shown are estimates only. Please see our partners for more details. Full view. View all photos A haven of peace in the city center, the hotel occupies a beautiful traditional mansion dating back to Furniture and antiques found in the capital here and there, then restored, rub shoulders in an atmosphere full of history. The architecture of the hotel is remarkable: while keeping the codes of Hauts-Plateaux, the house is quite exceptional because it benefits from very large volumes, which provide visitors with a sense of ease and well-being.
From some rooms upstairs, you can enjoy a nice view of the Royal Hill and the plains. The hotel Le Pavillon de l'Emyrne is located in the heart of the old town in a busy area full of trendy restaurants. Equipped for both family and business stays, this intimate hotel aims to make your stay in Antananarivo memorable.
Read more. Property amenities. Free parking.
Secure Online Dating Services in Madagascar
Free breakfast. Books, DVDs, music for children. Airport transportation. Meeting rooms.
Breakfast buffet. Kids' meals. Shuttle bus service. Taxi service. Currency exchange. Non-smoking hotel.
LE PAVILLON DE L'EMYRNE - Prices & Hotel Reviews (Madagascar/Antananarivo) - Tripadvisor
Laundry service. Air conditioning.
Private balcony. Flatscreen TV. Room service. Non-smoking rooms. Family rooms. Smoking rooms available. Languages Spoken. Antananarivo Airport 8 mi See all flights. Rental Cars See all Antananarivo rental cars. Write a review. Traveler rating. Selected filters. All reviews offer free breakfast was excellent mini bar the ground floor comfortable beds excellent hotel stayed one night papillon city. Sapper wrote a review Oct Excellent Hotel. We stayed here for three nights and have no complaints at all about the hotel located central within the city and approximately 40 minutes from the airport.
The staff are friendly and helpful, the rooms are clean, spacious and comfortable with all the usual facilities including wi-fi although the signal strength fluctuates. They have a mini-bar, laundry facility, safe, plenty of storage space and large comfortable beds. Breakfast facilities are on the ground floor with the adjoining restaurant serving good, reasonably priced meals. An ATM is a five minute walk away. Watch out for street beggars as they are quite persistent and try all the tricks in the book to get some cash.
Date of stay: October Trip type: Traveled as a couple. Helpful Share. London, United Kingdom 1, contributions helpful votes. The room was huge and very nice. The director and staff are incredibly friendly. They offer free massages. The breakfast was excellent. Highly recommended. Date of stay: August Trip type: Traveled with family. CaroPen wrote a review May Malborough, United Kingdom 2 contributions.
- Organising Your Trip;
- latin dating near Ogbomosho Nigeria;
- This start-up works like a dating site for therapy.
- lesbian dating in Pasto Colombia.
Lovely gem of a hotel - would highly recommend. I often travel to Madagascar for work and have now stayed in this hotel three times. Staff are really friendly and nothing is too much trouble. The ensuite rooms are spotless with air conditioning, a safe and mini bar. Breakfast has a wide selection of fruits, juices, pastries, omelette, crepes etc. There is also a lovely little restaurant serving French cuisine in the evenings.
When this is closed, there's a great creperie a few doors down. I would highly recommend this hotel to every weary traveller - a hidden gem tucked away on the slopes of Antananarivo. Date of stay: May All samples collected occur in the alluvium formation. All samples were collected in plastic polyethylene bottles: mL bottle for water-stable isotope 2 H, 18 O analysis and mL bottle for tritium analysis. Tritium occurs naturally as reaction product between atmospheric nitrogen and thermal neutrons as per Eq.
It is a short-lived radioisotope, with half life of Group 1 samples have similar stable isotope content, indicating connection and continuous flow from AM1 to AM2. In Group 2, where samples were collected downstream of the landfill, the samples are paired according to their geographical locations: the pair AM10, AM11 , sampled in the western part of the landfill, has similar stable isotope content, highlighting hydrological connection between the sampling points.
The same is also true for the other pair AM3, AM9 , which was collected in eastern part of the landfill. However, AM10, AM11 and AM3, AM9 have different stable isotope compositions, indicating that the absence of hydrological connection and probably different groundwater recharge mechanisms.
With a water table of 1. The stable isotope composition difference is in agreement with the hydroisohypses map, which shows different groundwater flow patterns in the eastern and western parts of the landfill. Comparing Group 1 and Group 2, stable isotope data also lead to the assumption of groundwater flow discontinuity from the highly tritium contaminated groundwater to further downstream in the water points.
Such a discontinuity would hinder contamination to spread over into the aquifer. AM6, which is sampled at the extreme north of the study area, upstream of the landfill site. This suggests a continuous groundwater flow from upstream of the landfill site to AM1. AM14, which is sampled close to AM6, but is much more enriched in heavy isotopes than the latter sample. Besides, AM14 is isotopically identical to AM11, which was sampled downstream of the landfill.
This leads to the assumption of probable connection from upstream to downstream of the waste deposit site on its western side.
Antananarivo Tourism | Antananarivo Guide
This is, however, not in agreement with the groundwater flow pattern. Moreover, the different stable isotope contents of the water samples collected between AM14 and AM11 would rather indicate groundwater flow discontinuity, which could be explained by the presence of several emerging springs.
Examining the tritium data further in the discussion helps highlight the groundwater flow and the spread of the contamination into the aquifer system. The stable isotope composition of the dug well waters Fig. This suggests that the isotope composition of spring waters results from a mixture of condensed rainfall and infiltrated evaporated rainfall down to the aquifer the latter would be probably of minor proportion , which would emerge as springs.
Group 1 is noticeably distinguishable from Group 2 and Group 3 because of its abnormally high tritium activities. The values of Although the exact source of tritium is unknown in the study area, high level tritium containing items such as gaseous tritium lighting devices, exit signs, watches, or clocks Murphy et al. For Group 2, the tritium activities reflect a natural origin and the values greater than 1 TU AM10 and AM11 indicate recently recharged groundwater Farid et al. For AM3 and AM9, having, respectively, 0.
From his study on the permeability of various grades of sand and peat and mixture of these with soil and vermiculite, Garman found that compacted peat in layer of 0. For Group 3, the tritium activities also indicate natural sources and young ground waters, except AM4. The latter water sample was collected just upstream of the landfill and has a tritium activity of 0. Such a low value refers to old groundwater and indicates groundwater of different source. This infers the absence of continuous flow from upstream to downstream of the landfill.
ANDASIBE & THE RN7 TO IFATY | 12 DAYS/ 11 NIGHTS
The higher tritium activities in water samples collected downstream of the landfill compared to that collected upstream NW—SW direction likely confirm the previous assumption. The theoretical discussion showed different sources of tritium just downstream of the landfill site and further down from, that is from Group 1 to Group 2. While assuming that an exponential decay governed by the radioactive decay, Eq. For AM3 and AM9, such calculation leads to erroneous results, since their tritium values indicate mixture of old and young groundwater. From Eq.
Considering the tritium activities of the dug well waters from the contamination point AM1 to RIVA, the latter sample has the highest activity, implying that the River is likely not a discharge point, since tritium activity decays along the groundwater flow path.
This would discard the use of RIVA tritium activity as A o, since the dug well waters are likely to be recharged by infiltration of much less evaporated rainfall, as the stable isotope composition seems to indicate. Tritium activities of precipitation in Antananarivo are measured locally and a value of 2. Those values are very similar to the tritium activities of spring waters SA01 and SA05 2. This agrees with the stable isotopes contents of SA01 and SA05, which are also similar. The highest tritium activity of natural origin measured in dug well waters is 1.