Gulf of Hammamet at dusk

TRAVEL TUNISIA

A marvellous place we spotted whilst exploring the pool area of another hotel accommodation situated close to the Marina in Yasmine Hammamet during our stay there for a few days in June 2023.

The Vincci Lella Baya is palatial hotel with a stunning white exterior. Featuring traditional architecture and modern facilities, the hotel offers a prime position overlooking the Gulf of Hammamet, which comes under the, Nabeul Governate of Tunisia.

Putting Vincci Lella Baya on the map (click through the blue link to see the location on the live Google Map link):

We spent 10 days staying at another Hotel (Medina Belisaire Thalasso & Spa) around 10 to 15 minutes stroll from the Marina.

"(ANSAmed) - TUNIS, SEPTEMBER 26 - A team of Italian researchers will rebuild for the first time in Tunisia the exact botanical composition of an ancient garden inside an aristocratic villa from 2,000 years ago, starting with pollen." "The Nymfarum Domus, a luxurious "domus" from about 400 A.D., is situated at the centre of Neapolis in the Gulf of Hammamet, in the area of Nabeul."

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An earthquake measuring 3.2 degrees hit the Gulf of Hammamet in the Tunisian province of Nabeul The seismological stations of the National Meteorological Institute of Tunisia recorded an earthquake on Sunday in the Gulf of Hammamet.

The conservative Ennahdha party has come first in Tunisia's parliamentary election, according to an exit poll broadcast by state TV.

The poll by Sigma Conseil showed Rached Ghannouchi's moderate Islamist party would secure 17.5 percent of Sunday's vote, or 40 seats in the 217-strong parliament. It was followed closely by Qalb Tounes, a relatively new party founded by jailed media mogul Nabil Karoui, at 15.6 percent or 33 seats.

Hours earlier, Karoui, one of the two candidates to advance to Tunisia's presidential runoff vote that will be held next week - claimed in a statement that his party had come first.

"We are the most visionary, we want to break the old establishment," Samy Achour, a senior member of Qalb Tounes's political bureau, told Al Jazeera.

But if exit polls are anything to go by, not everyone appears ready to do so.

In an election day that came and went without much enthusiasm, voter turnout was expected to have been low - recorded at 23.49 percent at 2pm, six hours after the opening of the polls.

Sharan Grewal, a visiting fellow at the Brookings Institution who focuses on North Africa, predicted a lower turnout compared with the first round of Tunisia's presidential election last month, which stood at 49 percent. The main reason, he said, was that some of the supporters of Kais Saied, Karoui's opponent in the upcoming presidential runoff, "stayed home" as the academic had no party and "did not endorse any party or list".

"Several parties including Ennahdha ... tried to court his voters, but it remains to be seen how they did," Grewal added.

In Sousse, on the Gulf of Hammamet, one voter said he was the only person in a crowded coffee shop sporting a blue index finger - the telltale sign of those who had cast their vote. Elsewhere, Zohra Eltaief, a 65-year-old retired nurse, said she voted for list number two, of Abir Moussi's party. Moussi is often referred to as being nostalgic of the era of Zine El Abidine Ben Ali, who ruled Tunisia for 24 years before being toppled in a 2011 civilian uprising that forced him to flee. "Moussi is a lawyer and has been always involved in politics, she is the extension of Bourguiba and Ben Ali who were devoted to the country," Eltaief said. "Today, she is the only one who is able to stop the obscurantism of Ennahdha and its allies."

According to the exit poll, Karama, a conservative coalition led by lawyer Seifeddine Makhlouf, came in third with 18 seats, followed by the recently formed Tahya Tounes secular party led by current Prime Minister Youssef Chahed with 16 seats.

"As in 2011 and 2014, the winning party will need to form a coalition to gain a majority," Grewal said. "The big question here is whether that coalition will include both the top two parties, Ennahdha and Qalb Tounes. During the campaign period, both ruled out a coalition between them."

This, says Grewal, could mean weeks or even months of negotiations. "No party has over 20 percent, and it will take at least four parties to even form a government," he added.

Sarah Yerkes, a fellow in Carnegie's Middle East Program, said she did not expect Ennahdha and Qalb Tunes to work together.

"If Ennahdha is asked to form a government, it will likely do so with a variety of smaller parties and independents," she said.

Yerkes added that if the exit poll was confirmed, the relatively weak performance of the top two parties compared with the previous parliamentary election in 2014 highlighted "how much more divided the political scene is today". Five years ago, Nidaa Tounes came first with almost 38 percent of the vote, followed by Ennahdha with nearly 28 percent.

More than 1,500 lists and 15,000 candidates on Sunday ran for 217 seats, with registered political parties and independents vying for control of the single chamber.

While Tunisia is often referred to as the only success story to come out of the Arab Spring, the elections were held against a backdrop of spiralling food prices, inflation and more than 15 percent unemployment.

tunisians expected democracy would allow them to vote out corruption and rich parasites and vote in western living standards. what they found was that they could only vote for people willing to apply a series of different social mores but all willing to apply the same set of internationally imposed austerity measures. as a result, most have become disillusioned and don’t even want to bother voting.

Sousse, Tunisia: Sousse or Soussa is a city in Tunisia, capital of the Sousse Governorate. Located 140 km south of the capital Tunis, the city has 271,428 inhabitants. Sousse is in the central-east of the country, on the Gulf of Hammamet, which is a part of the Mediterranean Sea. Wikipedia

Hilton Signs With Societe Marhaba Beach to Open Hilton Skanes Monastir Beach Resort – Hospitality Net

Hilton Signs With Societe Marhaba Beach to Open Hilton Skanes Monastir Beach Resort – Hospitality Net

Hilton (NYSE: HLT) recently announced an agreement with Societe Marhaba Beach to open Hilton Skanes Monastir Beach Resort. The upper upscale Hilton Hotels & Resorts property will offer incredible beach-side vistas across the Gulf of Hammamet, as part of the new Palm Lake Monastir residential and commercial development and within close proximity to the historic towns of Monastir and Sousse. Hilton…

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#Repost @afrikya.tn @download.ins --- yet another depiction of the adorable union between ageless #Hammamet and her #Sea, side by side, as seen from inside a 1200+ year-old #Fortress, looking after #Tunisia's northern-eastern Gulf, through the lens of Helmi Aouamri (@child_of_the_tunis_) . Limitless Dreams! . . . #igerstunisia #weposttunisia #tunisiarising #TunisieMoiJYVais #TrueTunisia #touneslike #visittunisia #ThisisTunisia ‪#tunisialovers #Tunisie #Tunesien #Tunesië #tunisien #Tunez #Tunezja #Тунис #تونس#突尼斯#チュニジア  #Tunus #Tunisko #Tunezija #meer https://www.instagram.com/p/CA2NEIeBwaP/?igshid=5h6wfkbyn9yy

Sedimentary and Tectonic Control of the Eocene/ Lower Miocene Hydrocarbon Systems of the Gulf of Gabes Basin-Ggb in Tunisia Introduction In the Gulf of Gabes Basin (GGB), limestones in the El Garia (Ypresian) and Ketatna (Rupelian-Burdigalien) formations are gas and oil prone [1-5]. They are comprised of carbonate platforms on which sedimentation, eustasy, tectonics and interrelated subsidence have exerted important controls. They were deposited in a lithotectonic setting dominated by two major orogenic phases, the Pyrenean and the Alpine. The former enabled collision of the North African plate margin against its Apulian counterpart [6-9] the initiation of the Tethys closure, the erection of the so-called box-folds and subsequent emersion of the Saharan Atlas [10]. The benthic El Garia and Ketatna Formations and the respectively coeval but pelagic Boudabbous and Salammbo Formations extend in a broad area covering the gulf of Hammamet, gulf of Gabes and Pelagian Block in the Southeast Tunisia [1,2,5,11]. Detailed petrographic and petrophysical studies of the limestones building the El Garia Formation have shown these series form commercial reservoir in the Ashtart, Cercina, Chergui, oil fields. Furthermore, the study of petroleum system series in the GGB help decipher a stratigraphical scenario of repetitive benthic carbonate platforms stacked in the sequence of stratigraphic ages, fitting laterally and upwards into pelagic counterparts. The Eocene El Garia reservoir settled in a broad area in the southwest of the GGB in continuity with the NW-SE directed Nummulitic ridge, passes laterally to the northwest into the Boudabbous Formation, a source rock dominated by marly limestones and black shales highly enriched in marine kerogen. This complex is sealed by a thick shaly Cherahil Formation, which in turn is transgressed over by a repetitive benthic but moderately to highly thick limestone packages in the Ketatna Formation. The latter broadly covers the proximal areas in the GGB, Pelagian Block and gulf of Hammamet, and fits laterally into its pelagic counterpart the Salammbo Formation which consists of rather marly deposits interceded with limestone beds. Moreover it is likely that increasing tectonic subsidence which might have dominated in the study area during the Lower Miocene has caused the marls and black shale deposits in the Salammbo Formation prograde over and seal the Ketatna limestone reservoirs. Based on recent fieldwork, stratigraphic data, well results and wire line log details, and seismic data, the main aim of this study is to demonstrate the close time/palogeographic relationships and configurations of these two major and superposed petroleum systems in the GGB covering a time span from the Eocene to the Lower-Middle Langhian times. The major constraints on the lithotectonic evolution, differentiation of sedimentary deposits and basin geometry are also examined in the light of sismostrati graphical and sismotectonic interpretations. The modeling approach help decipher benthic carbonate platform- and pelagic depositions, paleoeustatic changes in sea level, tectonics and inter-related subsidence, and as a consequence reservoir quality and source rock formation and maturation in the study time interval. This help us better contribute to the knowledge of the economic potential of the Eocene to Langhian series in the GGB. Go to Results And Discussion According to previous works, the Atlassic domain [12-14] and Sahel area [15-17] as well as the entire study area [4,11] were subjected to a dominant transpressive tectonic period beginning in the Santonian and ending in the early Paleogene with local East-verging reverse faulting identified in Santonian series of the Sahel area [17] During this period, transpressional move southeastwards exerted on transverse regional faults (E- W, S-N and NW-SE), has created rhomb-shaped and rotating blocks [18] with dominant low stand follows by a transgressive (TST) benthic carbonate sedimentation deposited in peritidal to infratidal milieu as indicated by frequent hummocky cross stratifications. These series have formed during the entire Senonian and have covered broad anticline structures and fault- bend folds. However, the latter were trimmed by depressions and remarkably subsiding tectonic troughs which have been in filled by the Upper Maastrichtian-Paleocene marls of the El Haria Formation. Click here to view Large Figure 1 The Ypresian to Lower Lutetian was a period of intense tectonic activity with dominant transpression directed NW-SE. In the Atlassic domain and Sahel area, tectonic deformation caused local uplift and erosion, continental/lacustrine sedimentation on emerged blocks and has initiated the Atlassic box and salt-cored folds directed majorly NE-SW [11,12,19]. In contrast, no clear folding features have been observed in the study area. Instead, the tectonic framework includes a dominant tilted morphology with ramp-shaped and uplifted blocks sur imposed to a network of normal faults directed majorly NW-SE and faced NE, but conjugated with additional regional sutures, S-N and particularly E-W in strike. This paleogeograpic style has closely controlled the Lower Eocene sedimentation. Indeed, during the Ypresian and Lower Lutetian, the ramp-shaped blocks were the sites of benthic carbonate deposition and enrichments in coarsened for aminifered tests (Figure1). The Ypresian to Lower Lutetian platforms include carbonate sequences deposited in a Transgressive Systems Tract during a period of sea level rise. These deposits may rest disconformably over the older El Haria and Abiod Fms sequences. Towards the Jeffara mole, the Eocene Group (Chouabine and El Garia Fms) fits laterally into the Tanit Formation which comprises shales and dolomites deposited in a shallow, presumably lagoonal environment, whereas, to the northeast, in the deeper basin parts, this Group passes laterally to thick pelagic series of bituminous black shales and lime mudstones enriched in Globigerinids in the Boudabbous Fm. The Ypresian to Lower Lutetian transpression was followed by a period of dominant subsidence and basin fill by remarkably thick, shaly and carbonate series of the Cherahil Fm which may rest disconformably over older deposits of the El Garia, El Haria and Abiod Fms. The Cherahil Fm are shales and siliciclastics poor in faunal content, interceded by mollusk bearing limestones. In field outcrops, these are forth to fifth order sequences with dominant shaly strata at the base shallowing upward into Bryozan, Mollusk and Ostrea- rich limestones. The Cherahil/ Souar shaly series provide seals for the oil prone El Garia Fm reservoirs and subdivide into three main Members: the so-called lower Cheral/Souar A and Upper Cherahil. Souar B separated by the middle Reineche Member formed by lime mud to wacke stone containing mainly Nummulites. The latter horizon, picked in seismic limes, could represent a Lutetian TST even if tectonic transpression, folding and uplift would be accompanied by bottom elevation and subsequent carbonate deposition in the photic zone. Indeed, tectonics is thought to have intervened and enabled the Cherahil Fm present local gaps and rest disconformably over the Maastrichtian Abiod, El Garia and EL Haria Fms. During the Rupelian to Burdigalian period, carbonates and marls prevailed with a clear disparity between platform and basin deposits. In the carbonate platforms, a basal Rupelian Horizon, 2 to 20m thick is easily picked in seismic lines in the Sahel, Pelagian Block and study area and is described as the lime wacke/packstones enriched in Nummulites vascus. It retraces a retrograding TST during the Early Oligocene, and passes upward to a highly thick carbonate series the strato type of which was described by Fournie in the Ketatna well. The series include lime mudstones and wacke/packstones enriched in coarse grained for aminifered tests, Nummulites, Bryozoans, Echinoids, Mollusks and Corals, dolomite beds and clay intervals. At the Jebel Abderrahman, Lower Oligocene limestone packages appear stratified, admit marl intercalations and display a similar faunal content [20,21]. In study area, the Ketatna Fm deposited to the west on a broad platform rimming a local basin centered on the gulf of Gabes. The geometry of the Rupelian-Burdigalian deposits was dictated by deep-seated and reactivating shear faults directed NW-SE, S-N and SW-NE, with antithetic branches. Due to prevalently trans tensional move of these flower-faults almost NW-SE in azimuth and with dominant vertical offsets, polygonal blocks organized in stacked ramps have formed, among which the most uplifted were the sites for benthic carbonate facies of the Ketatna Fm with clear shallowing up features on paleohighs. In contrast, subsiding blocks have formed graben and half graben basins always in filled by pelagic shales, marls and embedded lime mudstones of the Salammbo Fm. The latter may disconformably overlie the Boudabbous, the Abiod and the Doubled Formations. Also, in the Oil wells, the Ketatna Fm transgresses the El Garia and Double Fms respectively Thus, the basin framework during the Rupelian-Burdigalian times, responds to those continuously reactivating shear zones inter-related with the older Upper Cretaceous-Lower Paleocene and Upper Eocene tectonic phases. This is clearly evidenced by the lateral variations in facies and total thicknesses of the Ketatna and Salammbo Fms, but also by the facies inversions and interpenetrations thus forming a transition zone between these formations. The transitional lithofacies are dominated by an admixture of marls and carbonate deposits as observed in wells and in seismic lines cutting across the Ashtart oilfield, with flower faults and discontinuous hummocky cross-stratified seismic facies. The seismic facies reconstruction and extension of the platforms of El Garia and Ketatna are complex. In the internal ramp area of the two platforms of El Garia and Ketatna, seismic reflections are continuous, high amplitude and concordant; this can be explained by stacking carbonate seismic reflectors; however, the frequency is often low, so that reflections are subparallel configurations resulting spatiotemporal continuity of carbonate sedimentation. The seismic facies of the middle ramp variables are generally characterized by discontinuous reflections are strong amplitudes and sometimes clearly arranged in parallel or sometimes chaotic. The external ramp is cut by seismic reflections that offer high amplitude, discontinuous, sometimes heckled with an oblique configuration or hummocky (Figure 2). Click here to view Large Figure 2 The findings ofthe study based on the well to well correlations enhanced by logging analyzes, information obtained from the 3D seismic picking of seismic horizons and conversion in depth from Oil well data, stratigraphically well defined, and delineation of facies by discontinuities and sequences hiatus, gives Fms El Garia and Ketatna form of carbonate platforms. The respective periods of lithofaicies genesis, these platforms have recognized regional extension and were dislocated by regional dominant accidents NW-SE direction which was originally transpressive paleostress movements especially during the Maastrichtian, the Late Eocene, middle Miocene and Miocene-upper. These carbonate platforms seem to have been built in favorable photic conditions. The sedimentary floor may be relatively steady incline imposed on blocks cut by branched flowers faults that appear in the seismic profiles. Trends in bioaccumulations large foraminifera, including the Eocene and richness of carbonate productivity are indicatives of dominance of an environment beaten by the currents, well ventilated and oxygenated with absence of turbidity and away from detrital input. This type of environment supports Nummulites accumulations installed on the platform depth sloping shaped carbonate ramp built during the lower Eocene, then later repeated with the same intensity of productivity carbonates and explosion biological diversity in marine shallow during the Oligocene-Miocene. Successive sedimentation periods, was also conditioned by two factors: tectonics and eustasy. The tectonic factor contributes to the fragmentation of the blocks, their tilt; and in the distal area, subsidence basin with a marked change in the sedimentation represented by the micrite and pelagic deposits nature. Thus, by collapse of blocks of El Garia Formation is relayed by the facies of the Boudabbous Formation, and Formation Ketatna by pelagic deposits Salammbo Formation. Similarly, the above figures show that it is practically the same rooted accidents that have structured the Eocene sedimentary floor and controlled spatial and temporal distribution of deposits, by replaying the Oligocene- lower Miocene to impose similar palaeogeographical limits and almost at the same place of transition between Fm Ketatna and Salammbo Formation. Tracking facies described using cuttings and cores from boreholes clarifies the facies distribution and to recognize the characteristics of three distinct environments facies usually described for carbonate platforms ramp shaped [22-24]: internal ramp facies (inner ramp), the middle ramp facies low bathymetry (mid-ramp) and outer ramp facies (outer-ramp) depth seaward up the talus [18,23,25-27]. Finally, eustatisme also involved in instaurations of retrograde transgressive deposits like those of Reineche, Ain Ghrab and Melqart marking a remarkable extension of carbonate platforms in response to accelerated in the average level of sea rising. In the major parts of the basin of GGB faulting and subsidence controls on sedimentation. We found the deep effects of tectonics in the heightening blocks, deformation and sealing unconformable. The most common events were those Maastrichtian-Paleocene transition with the creation of bald areas in the NW part of the field of study and particularly in the Sahel of Sfax [16]. Dynamic events largely affected the series were also identified through the well data to higher-Priabonian Eocene to Langhian-Serravallian, then the passage of the Group Oum Douil Fm Somaa preceding the transgression of the limestone Fm Melqart and continentalization corresponding to laguno-lacustrine deposits Fm Oued Belkhédim. Carbonated systems associated with the development of a carbonate sedimentation on rhombic blocks which can be controlled by the eustatisme; but such carbonate sedimentation with an environmental dimming internal platform type to external platform environments. The deposits are thick and have lateral facies transitions with equivalent formations formed in the pelagic environment in abyssal conditions. We also noted the repetition over time of this type of sedimentation especially the ypresienne time (Fms El Garia/ Boudabbous) and later during the Oligocene-Burdigalian (Fms- Ketatna Salammbo). When comparing the zonal distribution of one and the other of these formations, and taking into consideration the well data and literature information, we realize in the study area, it is the same tectonic lineaments that have worked at successive periods to score quite deeply lithology series along paleogeographique transition lines passing between paleogeographic areas kind of training and different environment. The results of the seismic analysis enhanced by well logging allowed to recognize the architecture of the sedimentary cover at different times and to establish the relationship between litho stratigraphic formations (lateral facies passages), but also amongst tectonics and sedimentation. The major tectonic style is the continuity amongst a deep tectonic affecting the basement, which witnesses have been described by the authors in Medenine and Jeffara area [28,29]. We demonstrate that old tectonic dating to the Paleozoic and early Mesozoic is transmitted into the sediment cover. These manifestations are ramified to flowers faults that reactivated at different epoch. The major trending faults NW-SE to NS most often play slide ably with escarpments often looks NE, dislocated and raised of blocks and basins in grabens and half-grabens, very similar of what is commonly described by the authors on the continent in Central of Tunisia and in the chain of Chotts. The research of the discontinuities amongst sequences linked to the main geodynamic events that have controlled the basin sedimentation helps to clarify the geometry and the Seismic-sequences cutting series. Thus, it is possible to correlate the seismic super sequences to what is known in regions in central Tunisia as sedimentary megacycles identified by the authors regionally. In previous work [30,31], we found a great similarity in the distribution of deposits platforms and those pelagic equivalent, but at different ages as the Ypresian and Oligocene-Miocene epoch. We also showed the precise controls of eustatisme, reactivation of tectonic deep accidents, and morphology of the basins (platform, abyssal areas, shoals, emerged edges of blocks) in the differentiation of carbonate sedimentary environments [32-35]. Thus, it clearly shows by geophysical profiles in Ashtart province, on the vast field of the Pelagian block, the range of platforms (internal, intermediate and external shelf) and transitions to pelagic abyssal domains (basins) at the Ypresian (Formations Jebs, Metlaoui, El Garia, Boudabbous) and Miocene- Oligocene (Formations Messiouta/Fortuna, Ketatna Salammbo) are controlled by the same tectonic lineaments reactivated by ramified faults (flower structure) and sliding at different epochs [36-38]. Cutting blocks, the heightening local, also the subsidence allows the installation of carbonates platforms ramps environments in which carbonates productivity is provided by large foraminifera as Nummulites the Operculines the Discocyclines for Ypresian strata but also by Nummulites, the Amphistegines lepidocyclines and in the case of deposits of Oligocene-Miocene. These carbonate platforms ramps often isolated because of dislocated tectonic blocks. These ramps are distally deepened (distally steepened) and rarely bordered (rimmed shelves) (Figure 3) [39-41]. Click here to view Large Figure 3 Go to Conclusion As we mentioned in the case of the Permian, this architecture division of the Southeast margin of Tunisia during the Permian, Triassic, Jurassic, Cretaceous and as demonstrated in this work for the Cenozoic, is controlled by ancient tectonic directions affecting the basement [29], has always supported the development of carbonate platforms and bio constructions. It is therefore the same environmental control factors and sedimentation at different periods, produce the same effects. However, more NE and north, block subsidence allows the establishment of a frank pelagic sedimentation, where the lateral transitions in bathymetry conditions contrast between El Garia Fms/Boudabbous and Ketatna/ Salammbo. The interest and petroleum implications of these formations is the tectonic dynamic controlled the genesis of carbonate facies platforms ramp, but also their subsequent deformation: the El Garia Fm was distorted by tectonqiues Pyrenean deep reactivated movements during the Lutetien -to Priabonian, and Fm Ketatna by Alpine movements dating from Langhian-Serravallian. The deformation of the blocks and their emersion promotes the effects of the diagenesis dolomitisante enhances the porosity and permeability of such reservoirs; while the tectonic enhances fracture porosity and permeability. Moreover, reservoirs in contact with older source rocks (Bahloul, Fahdene, Aleg, El Haria, Tselja, Chouabine), but also with contemporary source rocks (Fms Boudabbous/El Garia and Salammbo/Ketatna) and the existence of thick clay layers forming impermeable seal against of oils migration (Fms Souar, Fm higher Salammbo; Oum DOUIL Group), offer a real opportunity for improving national reserves on hydrocarbons. Go to Acknowledgment This work gained financial support from the Ministry of High Education and Research (Tunisia). Constructive criticism of the Petroleum Research (ETAP), for data donated and compiled in this paper. Also, thanks to the SEREPT Company for Scientific support. For more Open Access Journals in Juniper Publishers please click on: https://juniperpublishers.com/ for more details click on the juniper publishers material science Science Juniper Publishers Materials Science Composite Materials Biological Engineering

سوق نابل المفتوح

سوق نابل المفتوح #السوق،#تونس،#سوق_تونس https://ift.tt/2GGZ2Xt سوق نابل مع اهتمام مستخدمي الانترنت في دولة تونس ونشاط البيع والشراء علي مواقع التواصل وبالاخص الفيس بوك للشعب التونسي تم انشاء صفحه خاصة في مدينة نابل لتسهيل علي الاخوه والاخوات البيع والشراء بكل سهوله ونشر اعلاناتهم مجانا عبر الصفحه الخاصة بهذه المدينة اهتمام الصفحه سوق نابل المفتوح في التالي مثال سوق نابل المفتوح للعقارات سوق نابل المفتوح للسيارات سوق نابل المفتوح للجوالات سوق نابل المفتوح للكمبيوتر سوق نابل المفتوح لغرف نوم والاثاث المنزلي سوق نابل المفتوح للطيور سوق نابل المفتوح للوظائف سوق نابل المفتوح للملابس سوقنابل المفتوح زيارتكم شرف لنا أهل نابل الكرام علي الرابط التالي الرابط للصفحه https://ift.tt/2Nk1tzE -------------------------------- تعريف موقع مدينة نابل التونسية مدينة نابل يحدها من الجنوب خليج الحمامات ومن الشمال عين كميشة ومن الشرق بني خيار ومن الغرب المرازقة مساحة نابل تقدر ب 2788 كم² عدد السكان حسب الاحصاء 73,128 (2014) Souk Nabeul With the interest of Internet users in the state of Tunisia and the activity of selling and buying on the sites of communication, especially Facebook for the Tunisian people A special page has been created in the city of Nabeul to facilitate the brothers and sisters selling and buying easily and publish their advertisements for free Via the city page Interesting page Nabeul open in the next Example Nabeul open real estate market Nabeul open market for cars Nabeul open market for mobile phones Nabeul open market for computers Nabeq open market for bedrooms and home furnishings Nabeul open market for birds Nabeul open market for jobs Nabeul open clothing market The open market Your visit is an honor to us the noble people of Nabeul on the following link Link to the -------------------------------- Definition of the city of Nabeul, Tunisia The city of Nabeul is bordered to the south by the Gulf of Hammamet, to the north by Ain Kemisha, from the east by Bani Khaylar and from the west by Mazraqa The area of ​​Nabeul is 2788 kilometers² Population According to Statistics 73,128 (2014) https://ift.tt/eA8V8J

JORDAN ON THE WEEKENDS

The Dead Sea Panoramic Complex/Dead Sea Museum is a new complex of regional museum about the Dead Sea, panorama lookout, restaurant and conference hall on a steep cliff high above the Dead Sea near Hammamet Ma'in it is accessible from both the Dead Sea and Madaba by car. The museum is run by the Royal Society for the Conservation of Nature, and has some fascinating information about the geology, ecology (animal and plant), archaeology, history and industry of the Dead Sea and surrounding area.

On the Jordanian side, the Dead Sea is possible as a day trip from both Amman and Aqaba. The road is a good dual carriage way. Tourist areas are accessible from the main road that runs along the eastern side of the body of water and connects to Jordan's Desert Highway running to Amman. Highways leading to the Dead Sea are clearly marked by brown tourist signs. It is an ambitious 3-hour drive from Aqaba in southern Jordan.

For relaxation, water sports, and winter warmth, Aqaba is warm, sunny and inviting, fringed with palm trees, lapped by the crystal clear waters of the Gulf of Aqaba, cooled by a steady northerly breeze, and ringed by mountains that change in color with the change of the hours. 

Located in the heart of Wadi Rum protected area, each tent is completed with comfortable beds, Bedouin sofa, mirrors, lamps, and the finest bed linens. There is cosy relaxation area outside the tent to watch the stars at night. Each tent has a private terrace with a fantastic view over the Wadi Rum Mountains. In the Wadi Rum Night camp, guests will find tents with a restaurant and lounge area. The tents is beautiful decorated with traditional Arabian furniture.

73 km (45 miles) north of Amman, and a short journey northwest from Jerash, through a beautiful pine-forest and olive groves, brings you to the town of Ajloun, where emperor Hadrian stayed over the winter of 129-30 AD, and built himself an arch well outside the town, leaving unbonded its sides for future city walls to come out to meet it.

Top 10 Must-See Places When Visiting Tunisia

Small and soft-particle white sand beaches are what attract millions of footprints every year to Tunisia. Sun-sand-and-sea holidays are a great escape from European cold winter. However, Tunisia has more to offer than its pristine beaches. We have provided the top-10 places to see in Tunisia so that you can have an easier trip.

10. Cap Bon Peninsula

Cap Bon Peninsula has the prettiest beaches in Tunisia. It lies on the north-eastern tip of the country. It is characterized by plenty of sun-drenched beaches, sweet-smelling jasmine flora, clear dark-blue sea, fragrant eucalyptus trees and thermal springs, among others. It is famously referred to as ‘the garden of Tunisia’.

9. The Ruins of Carthage

Carthage represents one of the oldest civilizations in the Maghreb region. It is a place where Phoenicians established their capital city and conquered other North African territories. Visiting Carthage will enable you to witness Roman ruins of Carthage.

Carthage is an important historical center in the Biblical history as some of the famous Biblical writers and figures and many other Christian adherents had their origin in this place. One of the living historical Christian landmarks is the Acropolium Church, which is one of the oldest and largest churches in North Africa. It is formally known as Saint Louis Cathedral.

Carthage was the capital city of Phoenicians and later on the Romans. It was a Roman palace in the South with picturesque gardens, Antoni baths, and Punica Ports.

8. Bardo Museum

Located in Tunis, Bardo museum houses some of the world’s famous mosaic collections. It has bits and pieces collected from every historical site in Tunisia. This is a place to visit should you desire to witness the intricate authentic artistry of the Roman and Byzantine eras.

Prior to Tunisia’s independence, Bardo Museum was a palace of the king of Tunisia.

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7. Sidi Bou Saidi

Sidi Bou Saidi is the most famous artistic village in Tunisia. Here you can be able to observe a village designed based on Tunisia’s finest village architecture. Sidi Bou Saidi is a clifftop village exhibiting whitewashed alleys, colorful blue doors, and wrought-iron window frames. Within it and its vicinity are stalls selling artistic craftwork where you can buy your own souvenir in memory of your visit to this great architectural village.

Sidi Bou is named after a famous Muslim cleric. It is just 10 kilometers to the western side of Tunis. Being on a hilltop area, it affords tourists a magnificent view of the Mediterranean sea.

6. Kairouan

Kairouan is the fourth most important holy city of the Muslim faith. It is a collection of madrassas, mosques,  and tombs. Bulky domes and skinny minarets are a testimony of the inspiring Arabic architecture. The city’s medina characterized by its maze-like narrow lanes and colorful near-crumbling ancient houses are a sight to behold. It makes you feel the ancient sensations of a great civilization.

Just 107 kilometers away from Kairouan is Sebetila which is home to Capitoline temple and other Roman relics. It is popularly referred to as Byzantium Roman Culture center. It attracts tourists across the world, mostly from Europe and those of the Roman Catholic faith. Since it is less than 2 hours drive, most tourists stay at Kairouan while on a visit to the place.

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5. Monastir Ribat

Monastir is a beautiful seaside resort city in Tunisia just 160 kilometers from Tunis. It is strategically positioned at the tip of a small protruding peninsula between the bay of Al-Manastir and the Gulf of Hammamet. It has a long stretch of golden sand beaches waved by restful blue sea. Monastir is reputed for being the ancestral home of Tunisia’s first president Habib Bourguiba and two former prime ministers – Hedi Amara Nouira and Mohamed Mzali.

Monastir was a heavily fortified city in ancient times. Most of the fortified buildings have collapsed except the Ribat fortress. Ribat is among the ancient string of defensive forts that protected the coastline from foreign intrusion. It is a beautiful thick-walled golden-stoned fort overlooking the harbor. It is one those sites that are sought for filming and features in some of the famous movies.

4. El Djem Amphitheatre

Probably the most cited of all tourist attractions when it comes to advertisements, El  Djem Amphitheatre is one of the largest in the world. It is three-tier high Roman amphitheater and has underground compartments. The underground area, once the home of the gladiators, is still intact with its various dungeons and tunnels.

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3. Nabeul, Hammamet

Thousands of tourists flock Nabeul every year. Its main attraction is the plenty of handicrafts. Also, its history as the administrative capital of the ancient Mediterranean citizens who have been natives since the Roman era attracts many to experience its authentic culture. Nabeul is located just about 20km from Hammamet.

Hammamet itself is a fishing town famous for its beautiful beaches. It is widely known for swimming and water sports. Its spectacular and serene picturesque characterized by green surroundings, fresh air, and soothing ambiance make it highly attractive to nature tourism.

2. Sousse Medina

Sousse is Tunisia’s third largest city after Tunis and Sfax. It is famous for its olives and olive oil production. It is just about 12 miles from Monastir. High nightlife characterized by bombastic nightclubs make it one of the best entertainment tourism sports in Tunisia.

Sousse Medina is a former military port located at Tunisian coast. It is a UNESCO world heritage site dating from the early centuries of Islamic adventure into North Africa. One famous mosque is the Ftata mosque. Apart from the ancient historical sites, Sousse is well-known for its beautiful, clean and serene sandy beaches.

 1. Grand Erg Oriental

Sahara region offers tourists a spectacular view of Sahara Desert. It also gives a glimpse of the nomadic pastoralists way of life. Camels are the most important animals in this environment as they are not only a means of transport but also a means of entertainment during Camel derby.

The contour-patterned sand dunes are just an amazing sight to behold. Scenes from English Patient Star Wars were once filmed from this place.  Nefta is an epitome of beautiful sand dunes while Chot el Jerid is a vast salt lake.

Conclusion

Tunisia is a place you would wish not to miss on your trip to Africa and the greater Mediterranean region. It has great attractions that will leave you with unforgettable memories that you will always cherish. Make an effort to have these 10 destinations on your list of places to see in Tunisia

The post Top 10 Must-See Places When Visiting Tunisia appeared first on Afrikanza.

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#landscape #aurora #dawn #sky #blusky #aircraft #aviation #airport #summervibes #lifestyle #lifeisbeautiful (at Gulf of Hammamet)

Hammamet La Badira Enjoy one of our legendary sunsets over the Gulf of Hammamet from the Georges Sebastian pool !🌴🎴 #LaBadira (à Hammamet, Tunisia) https://www.instagram.com/p/B0uD6L1BSUE/?igshid=bowxg6yexvis

From @the.peanut.vendor via @beau_traps in beautiful Hammamet in my Tunisia "A low key terrace of a Tunisian seaside villa, overlooking the Gulf of Hammamet. It’s supported by sections of locally excavated Roman columns. Might try and recreate this on regents canal 🙃" https://www.instagram.com/p/Bz-7uNShztj/?igshid=1l44kjow5usrw