1,355,282 research outputs found
Adare Manor: Tasting Menu
No full textAdare Manor is a five star hotel and golf resort located in the picturesque village of Adare in Co. Limerick. The house is set on a 840-acre (3.4 km2) estate and now operates as a five star hotel, featuring the Adare Golf Club, Lavender Cottage, Townhouses and Villas on the rest of the resort. President Bill Clinton stayed in Adare Manor in September 1998. The Manor was voted Ireland\u27s Leading Hotel at the World Travel Awards 2010, 2011 and 2012 and The World\u27s Leading Boutique Golf Resort in 2012.It offers a number of dining experiences from fine to more casual dining.
Hotel website available herehttps://arrow.tudublin.ie/menus21c/1066/thumbnail.jp
Adare Manor: à la Carte Menu 3rd. of January, 2013
No full textAdare Manor is a five star hotel and golf resort located in the picturesque village of Adare in Co. Limerick. The house is set on a 840-acre (3.4 km2) estate and now operates as a five star hotel, featuring the Adare Golf Club, Lavender Cottage, Townhouses and Villas on the rest of the resort. President Bill Clinton stayed in Adare Manor in September 1998. The Manor was voted Ireland\u27s Leading Hotel at the World Travel Awards 2010, 2011 and 2012 and The World\u27s Leading Boutique Golf Resort in 2012.It offers a number of dining experiences from fine to more casual dining.
Hotel website available herehttps://arrow.tudublin.ie/menus21c/1067/thumbnail.jp
Restaurant 1826 Adare Dinner Menu 2017
No full textThe rustic cottage setting and chic country décor, paired with food offering freshness, simplicity and keen pricing to match, make a winning combination. Seasonal local produce is the foundation of Wade’s food philosophy, so menus change on a monthly basis, and there are blackboard specials such as whole sole, braised meats and so on changing daily. Signature dishes include: Warm Chicken Liver salad, with Piccalilli, pickles and Bally greens and Head to Tail Free Range Pork Tasting Plate. The thatched cottage restaurant that is 1826 Adare, gets its name from the year the first Lord of Dunraven, built the cottage. Situated in the picturesque village of Adare, Wade and Elaine strive to maintain the old world charm and character of the cottage, whilst offering you modern Irish cooking, matched with friendly and attentive service.https://arrow.tudublin.ie/menus21c/1403/thumbnail.jp
Restaurant 1826 Adare Group Menu 2017
No full textThe rustic cottage setting and chic country décor, paired with food offering freshness, simplicity and keen pricing to match, make a winning combination. Seasonal local produce is the foundation of Wade’s food philosophy, so menus change on a monthly basis, and there are blackboard specials such as whole sole, braised meats and so on changing daily. Signature dishes include: Warm Chicken Liver salad, with Piccalilli, pickles and Bally greens and Head to Tail Free Range Pork Tasting Plate. The thatched cottage restaurant that is 1826 Adare, gets its name from the year the first Lord of Dunraven, built the cottage. Situated in the picturesque village of Adare, Wade and Elaine strive to maintain the old world charm and character of the cottage, whilst offering you modern Irish cooking, matched with friendly and attentive service.https://arrow.tudublin.ie/menus21c/1404/thumbnail.jp
Geophysical Investigations of Near-Surface Structure on the Earth and Mars
No full textI use remote sensing and active seismic methods to investigate near-surface structure on the Earth and Mars. These studies provide insight into styles of crustal deformation acting on continental margins in regions of extension, as well as paleoclimates that shaped the polar ice caps on Mars. I map the overall structure of the ice-rich Planum Boreum deposit at the north pole of Mars using 178 orbits of Mars Advanced Radar for Subsurface and Ionosphere Sounding data, and find no deflection of the lithosphere beneath the ice load. Bright, laterally extensive subsurface reflectors in the radargrams define the surface underlying Planum Boreum, as well as the interface between the two main units, the stratigraphically older Basal Unit and the stratigraphically younger North Polar Layered Deposits. The volumes of these units, and the overall edifice, are determined to the greatest accuracy possible to date. On Earth, I use a GPS campaign network in the state of Jalisco to investigate tectonic motion and interseismic deformation in the area. The consistent magnitude and direction of station velocities on the Jalisco Block suggest that it is moving rigidly with respect to North America. We constrain extension across the bounding fault zones of the block to values that are slow compared to relative rates of motion at nearby plate boundaries. I study another continental rift zone, in the Ross Sea, Antarctica, with refraction seismic data collected during research cruise NBP0701. I construct velocity models from 71 sonobuoys that detect deep structure in the oceanic crust of the Adare Basin and the crust of the Northern Basin, which lies to the south on the continental shelf. We demonstrate the importance of using multi-channel seismic data to correct for ocean currents and changes in ship navigation, the finite-difference modeling techniques necessary for accurately determining 1D velocity profiles for each sonobuoy, and for tying true velocities to the multi-channel seismic images of subsurface structure. We construct 2D velocity profiles using widely spaced sonobuoys in the Adare Basin, and using overlapping sonobuoys along some lines in both basins, and across the shelf break, to investigate crustal structure in the region. Detection of the Moho at 5.5 km below the seafloor by one sonobuoy suggests relatively thin oceanic crust in the Adare Basin, and flat velocity contours across the margin suggest continuity in crustal structure between the two basins
Temperature curve at Cape Adare
No full textThis record was harvested from a previous catalogue system and will be withdrawn in 2025. Information in this record may be superseded or incomplete. Visit this record in UMA's new catalogue at: https://archives.library.unimelb.edu.au/nodes/view/246493A meteorological graph illustrating the temperature curve at Cape Adare, 4 May - 2 June 1911.
Inscription: 663116798
Item: [1980.0030.00839] "Temperature curve at Cape Adare
Cape Adare
No full textThis record was harvested from a previous catalogue system and will be withdrawn in 2025. Information in this record may be superseded or incomplete. Visit this record in UMA's new catalogue at: https://archives.library.unimelb.edu.au/nodes/view/246159Flat topped scree platform with beach and sea with ice floes in the background. Image taken by Frank Debenham during the British Antarctic Expedition 1910-13.
Inscription: 698116820
Item: [1980.0030.00505] "Cape Adare
Postspreading rifting in the Adare Basin, Antarctica: Regional tectonic consequences
No full textExtension during the middle Cenozoic (43–26 Ma) in the north end of the West Antarctic rift system (WARS) is well constrained by seafloor magnetic anomalies formed at the extinct Adare spreading axis. Kinematic solutions for this time interval suggest a southward decrease in relative motion between East and West Antarctica. Here we present multichannel seismic reflection and seafloor mapping data acquired within and near the Adare Basin on a recent geophysical cruise. We have traced the ANTOSTRAT seismic stratigraphic framework from the northwest Ross Sea into the Adare Basin, verified and tied to DSDP drill sites 273 and 274. Our results reveal three distinct periods of tectonic activity. An early localized deformational event took place close to the cessation of seafloor spreading in the Adare Basin (~24 Ma). It reactivated a few normal faults and initiated the formation of the Adare Trough. A prominent pulse of rifting in the early Miocene (~17 Ma) resulted in normal faulting that initiated tilted blocks. The overall trend of structures was NE–SW, linking the event with the activity outside the basin. It resulted in major uplift of the Adare Trough and marks the last extensional phase of the Adare Basin. Recent volcanic vents (Pliocene to present day) tend to align with the early Miocene structures and the on-land Hallett volcanic province. This latest phase of tectonic activity also involves near-vertical normal faulting (still active in places) with negligible horizontal consequences. The early Miocene extensional event found within the Adare Basin does not require a change in the relative motion between East and West Antarctica. However, the lack of subsequent rifting within the Adare Basin coupled with the formation of the Terror Rift and an on-land and subice extension within the WARS require a pronounced change in the kinematics of the rift. These observations indicate that extension increased southward, therefore suggesting that a major change in relative plate motion took place in the middle Miocene. The late Miocene pole of rotation might have been located north of the Adare Basin, with opposite opening sign compared to the Eocene-Oligocene pole
(Table 1) Palynological investigation at DSDP Hole 28-274 north-northeast of Cape Adare, Antarctic
No full text(Table 1) Palynological investigation at DSDP Hole 28-274 north-northeast of Cape Adare, Antarcti
Seismic stratigraphy of the Adare Trough area, Antarctica
No full textThe Adare Trough, located 100 km NE of Cape Adare, Antarctica, is the extinct third arm of a Tertiary spreading ridge that separated East from West Antarctica. We use seismic reflection data, tied to DSDP Site 274, to link our seismic stratigraphic interpretation to changes in ocean-bottom currents, Ross Sea ice cover, and regional tectonics through time. Two extended unconformities are observed in the seismic profiles. We suggest that the earliest hiatus (early Oligocene to Mid-Miocene) is related to low sediment supply from the adjacent Ross Shelf, comprised of small, isolated basins. The later hiatus (mid-Miocene to late Miocene) is likely caused by strong bottom currents sourced from the open-marine Ross Sea due to increased Antarctic glaciation induced by mid-Miocene cooling (from Mi-3). Further global cooling during the Pliocene, causing changes in global ocean circulation patterns, correlates with Adare Basin sediments and indicate the continuing but weakened influence of bottom currents. The contourite/turbidite pattern present in the Adare Trough seismic data is consistent with the 3-phase contourite growth system proposed for the Weddell Sea and Antarctic Peninsula. Multibeam bathymetry and seismic reflection profiles show ubiquitous volcanic cones and intrusions throughout the Adare Basin that we interpret to have formed from the Oligocene to the present. Seismic reflection profiles reveal trans-tensional/strike-slip faults that indicate oblique extension dominated Adare Trough tectonics at 32–15 Ma. Observed volcanism patterns and anomalously shallow basement depth in the Adare Trough area are most likely caused by mantle upwelling, an explanation supported by mantle density reconstructions, which show anomalously hot mantle beneath the Adare Trough area forming in the Late Tertiary
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