bar&grill KASPIAN PALACE

Serving, composition and availability of dishes may vary, availability of dishes may be limited.

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  The Rychal-Su water originates from the melt waters of the Shalbuzdag mountain glacier, which penetrate into the deep layers of the earth, pass through many mineral layers, are enriched with macroelements, and, under the influence of natural processe
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  Water from the glaciers of Mount Kazbek, enriched with salts and minerals of the Caucasus Mountains, is a low-mineralized sulfate-hydrocarbonate, sodium-calcium water with an increased content of silicic acid.
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  Meltwater from the glaciers of the Main Caucasus Range has been passing through a natural filter for centuries, through the mountain mass, harmoniously enriched with useful microelements (such as Mg, Ca, Na), and emerges at the surface at the foot of
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  Meltwater from the glaciers of the Main Caucasus Range has been passing through a natural filter for centuries, through the mountain mass, harmoniously enriched with useful microelements (such as Mg, Ca, Na), and emerges at the surface at the foot of
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  Meltwater from the glaciers of the Main Caucasus Range has been passing through a natural filter for centuries, through the mountain mass, harmoniously enriched with useful microelements (such as Mg, Ca, Na), and emerges at the surface at the foot of
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  Meltwater from the glaciers of the Main Caucasus Range has been passing through a natural filter for centuries, through the mountain mass, harmoniously enriched with useful microelements (such as Mg, Ca, Na), and emerges at the surface at the foot of