— — a port the bora wind comes down to scour clean.
“A working port on the northeast Black Sea, set at the head of Tsemes Bay where the Markotkh ridge drops to the water. The bora, a cold downslope wind, comes through in winter at gale force. Long grain quays and tanker piers run the inner harbour. South of town the limestone cliffs of Abrau-Dyurso shelter a small wine country. The water turns slate when the wind pushes through. — from the studio
Each tile is finished by hand in our Knoxville studio. Artwork is slowly infused into the ceramic surface under high heat and pressure, and rests beneath a thin glossy finish. The colour lives in the surface, not on top of it.
Pick any four 4-inch tiles — National Parks you've been to, a Smokies set, the four seasons of one place. $ for a set of , cork-backed, ready to live on the table.
Novorossiysk is a city of around 270,000 in Krasnodar Krai, on the northeastern shore of the Black Sea. It sits at the head of Tsemes Bay, where the Markotkh ridge of the western Caucasus foothills drops to the sea. The city is Russia's largest commercial port by tonnage, handling grain, oil, and container traffic; the Caspian Pipeline terminal at South Ozereyka, about fifteen kilometres west, is one of the country's main crude-export points. Novorossiysk was founded in 1838 as a fortified settlement at the site of the Ottoman fort Sujuk-Kale.
The defining feature of the city's weather is the bora, a katabatic wind that pours off the Markotkh ridge into Tsemes Bay. Gusts above 40 metres per second have been recorded, and the bora can hold for several days, coating moored ships and quayside cranes in spray ice. Winters are otherwise mild for Russia, with January means near 3°C. The summer climate is warm-Mediterranean, with July highs near 28°C and a long dry season from June through September.
South of the city, the limestone cliffs around Abrau-Dyurso shelter Russia's oldest sparkling-wine estate, founded in 1870 under Tsar Alexander II to supply the imperial court. The Abrau lake sits at 84 metres elevation, a karstic basin held by the ridge. The Markotkh range itself is a section of the western Greater Caucasus, with peaks above 700 metres directly behind the city. The cliffs along the coastal road toward Gelendzhik show the same chalky limestone bedding seen across the northern Black Sea margin.