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I've been suffering for my art out in the garden trying to capture some moments from the snowy winter we've had this January!
Sinónimo: Racosperma hakeoides (A. Cunn. Ex Benth.) Pedley.).
Arbustos altos, tupidos, glabros y extendidos o pequeños árboles , de 1 a 5 m de altura; ramillas numerosas, ascendentes, lisas, pardo grisáceas, levemente angulares hacia el ápice.
Filodios estrechos, obovados, oblanceolados, 4-12 cm de largo, 3-12 mm de ancho, planos, gruesos, rectos o ligeramente curvados, vena media ligeramente excéntrica, venas laterales oblicuas, oblicuas y reticuladas, ápice generalmente obtuso con un pequeño color marrón rojizo glándula, una segunda glándula en el margen superior, generalmente justo debajo de la mitad de los filodios. Inflorescencias axilares y glabras, racimos a veces casi tan largos como filodes, que constan de 6-12 cabezas bastante densamente colocadas; cabezas de flores amarillas, globulares, c. 25 flores; pedúnculos cortos, extendidos, robustos, bastante gruesos, glabros; flores 5-meras. Legumbres lineales, de 7-10 cm de largo, 4-7 mm de ancho, moniliformes, curvas, café oscuro, ápice generalmente agudo; márgenes engrosados, marrón claro. Semillas longitudinales en la legumbre; funÃculo corto, engrosándose gradualmente en un arilo claviforme. Originario del sur y sur de Australia. se encuentra en la zona 8 en Iturraran.
Synonym: Racosperma hakeoides (A. Cunn. ex Benth.)Pedley.).
Tall, bushy, glabrous, spreading shrubs, or little trees 1-5 m high; branchlets numerous, ascending, smooth, grey brown, slightly angular towards the apex. Phyllodes narrow obovate, oblanceolate, 4-12 cm long, 3-12 mm broad, flat, thick, straight or slightly curved, mid-vein slightly eccentric, lateral veins obvious, oblique and reticulate, apex usually obtuse with a small reddish-brown gland, a second gland on the upper margin, usually just below the middle of the phyllodes.
Inflorescences axillary and glabrous, racemes sometimes almost as long as phyllodes, consisting of 6-12 rather densely placed heads; flower-heads yellow, globular, c. 25-flowered; peduncles short, spreading, stout, rather thick, glabrous; flowers 5-merous. Legumes linear, 7-10 cm long, 4-7 mm broad, moniliform, curved, dark brown, apex usually acute; margins thickened, light brown. Seeds longitudinal in legume; funicle short, gradually thickening into a clavate aril. Native to south and southern Australia. Area 8 in Iturraran.
Shot through the atrium ceiling at the Gaylord Texan Hotel and Resort just outside of Dallas, Texas. The hotel was near the Dallas/Ft. Worth airport, so there were lots of low flying planes over the grounds.
Angular Nude
by Koola Adams
Cubist Style Nude painting. Acrylic inks on paper. 40cm x 30cm
Frame and mount not included
Copyright reserved by the artist.
www.contemporary-artists.co.uk/paintings/angular-nude/
#art #painting #artists
One of the world's most impressive angular unconformities is located along Interstate 70 in Salina Canyon, central Utah. Angular unconformities are formed by structural tilting or folding of flat-lying sedimentary rocks, followed by erosion, followed by deposition of more flat-lying sedimentary rocks. The Salina Canyon angular unconformity includes outcrops of horizontal beds atop vertical beds. The overlying beds are basal Flagstaff Formation (mid-Paleocene). The underlying reddish-colored beds are tilted Twist Gulch Formation (Middle Jurassic) (also known as the Twist Gulch Member of the Arapien Formation).
The angular unconformity is exposed throughout the lower parts of Salina Canyon (Salina Creek valley), east of the town of Salina, on both sides of Interstate 70 (but better seen on the northern side of the highway). Eastward, the underlying rocks become less vertical (as seen in this picture), and eventually have a disconformable relationship with the overlying rocks.
The structural tilting of the Twist Gulch Formation has been attributed to local salt dome tectonics. Evaporites occur in underlying Middle Jurassic strata. Some of the rock salt intervals have domed upward as salt diapirs, resulting in tilting of overlying beds. The Salina Canyon angular unconformity provides information about the timing of rock salt diapirism (i.e., post-Jurassic & pre-Paleocene - in other words, during the Cretaceous).
The rocks just above the unconformity are sandstones, with some conglomerate lenses (basal lags).