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William Guidara (born 1979) is an American restaurateur based in New York City. Along with chef Daniel Humm , Guidara co-owned the Make It Nice hospitality group, established in 2011, which owns and operates Eleven Madison Park , NoMad New York , NoMad Los Angeles, NoMad Las Vegas, NoMad Bar and Made Nice.
In a statement, Meyer blamed the closure on the specificity of the Indian cuisine offered by the restaurant. [8] That same year, Meyer participated in a documentary called "The Restaurateur". [9] [10] In late 2011, Union Square Hospitality group sold Eleven Madison Park to its chef Daniel Humm and front-of-house director Will Guidara. [11]
The model displayed remnants of submerged plates located under oceans and in the middle of continents, which—according to our current understanding of the plate tectonic cycle—are all too far ...
Planetary scientists have not reached a consensus on whether Earth-like exoplanets have plate tectonics, but it is widely thought that the likelihood of plate tectonics on an Earth-like exoplanet is a function of planetary radius, initial temperature upon coalescence, insolation, and presence or absence of liquid-phase surface water. [3] [4] [5 ...
The restaurant, where Humm's prized dish is celery root cooked in a pig's bladder, has just extended its lease for another 20 years and will close for three months for an overhaul.
Surface map of oceanic crust showing the generation of younger (red) crust and eventual destruction of older (blue) crust. This demonstrates the crustal spatial evolution at the Earth's surface dictated by plate tectonics. Earth's crustal evolution involves the formation, destruction and renewal of the rocky outer shell at that planet's surface.
This era is marked by the further development of continental plates and plate tectonics. The supercontinent of Columbia broke up between 1500 and 1350 million years ago, [ 5 ] and the fragments reassembled into the supercontinent of Rodinia around 1100 to 900 million years ago, on the time boundary between the Mesoproterozoic and the subsequent ...
Forming the Atlantic segment of the boundary between the African and Eurasian plates, the AGFZ is largely dominated by compressional forces between these converging (3.8 to 5.6 mm/a (0.15 to 0.22 in/year)) plates, but it is subject to a dynamic tectonic regime that also involves extension and transform faulting.