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The name 'soumak' may plausibly derive from the old town of Shemakja in Azerbaijan, once a major trading centre in the Eastern Caucasus. [1] Other theories include an etymology from Turkish 'sekmek', 'to skip up and down', meaning the process of weaving; or from any of about 35 species of flowering plant in the Anacardiaceae or sumac family, such as dyer's sumach (Cotinus coggygria), used to ...
A red Cross of Saint James with flourished arms, surmounted with an escallop, was the emblem of the twelfth-century Galician and Castillian military Order of Santiago, named after Saint James the Greater. Saint Julian Cross: A Cross Crosslet tilted at 45 degrees with the tops pointing to the 'four corners of the world'.
Cross-bedding and scour in a fine sandstone (Logan Formation, Mississippian, Jackson County, Ohio) A teepee structure in modern halite deposits along the western shore of the Dead Sea, Israel. These structures are within sedimentary bedding and can help with the interpretation of depositional environment and paleocurrent directions. They are ...
Sand dune cross-beds can be large, such as in the Jurassic-age erg deposits of Navajo Sandstone in Canyonlands National Park. Aztec Butte shown here Formation of cross-stratification Schematic of eolian cross-bedding Close up of cross-bedding and scour, Logan Formation, Ohio Tabular cross-bedding in the Navajo Sandstone in Zion National Park Tabular cross-bedding in the South Bar Formation in ...
9th-century Byzantine seal showing a patriarchal cross (seal of Niketas, commander of the Byzantine imperial fleet) Seal of Bouchard de Marly (attested 1225), a cross, quarterly four alerions Seal of Amadeus V, Count of Savoy (1249–1323), showing a knight on horseback displaying the Savoy cross on his shield, ailets (shoulder-pads) and caparison (horse covering) A section of Segar's Roll, a ...
Hummocky cross-stratification from the Book Cliffs, Utah. Hummocky cross-stratification from the Arisag Formation (Silurian), Nova Scotia. Hummocky cross-stratification is a type of sedimentary structure found in sandstones. It is a form of cross-bedding usually formed by the action of large storms, such as hurricanes. It takes the form of a ...
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