Login

Datolite

Datolite - Bor Pit, Dal'negorsk B deposit, Dal'negorsk, Primorskiy Kray, Russia
Size: 12.2 x 4.6 x 2.3 cm

Very fine undamaged green translucent crystals of datolite to 2.7 cm in size are covering a chain-like matrix measuring 12.2 x 4.6 x 2.3 cm in size overall. Large crystals for the species with great color - an excellent example for this species!

 

Germany : Strange Agricultural Landscapes Seen From Space

"This agricultural area in midwestern Germany also features enormous opencast coal mines, one of which appears in the far right of this simulated-natural-color image, taken by NASA’s Terra satellite Aug. 26, 2000. Light green patches are crops, dark green is forest, grey is bare soil or urban areas, and the bright blue and white striped area is the mine. The mines in the area are worked by the Bagger 293, the largest machine in the world. The bucket-wheel excavator is twice as long as a soccer field and as tall as a 30-story building It digs up 30 million tons of lignite per year."  

 

Our Planet in Ecological Debt

an interactive infographic via chartsbin.com

 

Global Milk Production and Consumption


   

an interactive infographic via chartsbin.com

Snowflake (16X)

by Yanping Wang

 

Swirls, Gullies and Bedrock

"A new image from the HiRISE camera on the Mars Reconnaissance Orbiter shows an ethereal landscape...as dust devils move across the Martian surface and expose the underlying darker material."

 
"Dunes and bedrock near Noachis Terra on Mars."

 

 

Grand Teton, Mount Owen, and Uplifted Cambrian Shoreline

by Marli Bryant Miller  

"The above photo shows Mount Owen (left) and Grand Teton the two highest peaks in Grand Teton National Park, Wyoming. The Cambrian Flathead sandstone, shown here as the nearly flat-lying rock of the middleground, reflects encroachment of the ocean onto continental North America at the beginning of the Paleozoic Era about 540 million years ago. This sandstone crops out throughout the western United States, and includes the Tapeats Sandstone of the Grand Canyon. Beneath the sandstone lies much older rock, which in the Tetons is Archean gneiss and Proterozoic granite. The gneiss appears in the cliffs below the sandstone and in Mount Owen; the Proterozoic granite makes up most of the Grand Teton. The older rock of the peaks appears higher than the Cambrian Sandstone because of slip on the Buck Mountain fault zone during the late Mesozoic"

Mount Owen, Wyoming Coordinates  43.746944, -110.796667