domingo, 26 de março de 2017

Top Spots For Gem Hunting In The US

Top Spots For Gem Hunting In The US

1. Emerald Hollow Mine, Hiddenite, North Carolina

Find glittering, gorgeous emeralds in Hiddenite, only about an hour’s drive from Winston-Salem, NC. The Emerald Hollow Mine is home to the only emerald mine in the United States open for public treasure hunting. There are sluiceways where you can check out findings from the mine, or you can pay to do your own prospecting, digging, and hunting for a small fee.
Although the 70-acre site is known mostly for its emeralds, you could also end up with sapphire, tourmaline, garnet, topaz, and aquamarine. The mine is open year-round and boasts gorgeous scenery, too.

Gold

Gold

Gold Foresthill, Placer Co., California, USA Size: 2.3 x 1.3 x 0.5 cm (thumbnail) © danweinrich
Chemical Formula: Au
Locality: Sierra Nevada Mountains, Nome, Alaska and many other places in the world.
Name Origin: Anglo Saxon, of uncertain origin.
Gold is a chemical element with symbol Au (from Latin: aurum) and atomic number 79. It is a bright yellow dense, soft, malleable and ductile metal. The properties remain when exposed to air or water. Chemically, gold is a transition metal and a group 11 element. It is one of the least reactive chemical elements, and is solid under standard conditions. The metal therefore occurs often in free elemental (native) form, as nuggets or grains, in rocks, in veins and in alluvial deposits. It occurs in a solid solution series with the native element silver (as electrum) and also naturally alloyed with copper and palladium. Less commonly, it occurs in minerals as gold compounds, often with tellurium (gold tellurides).
Gold’s atomic number of 79 makes it one of the higher atomic number elements that occur naturally in the universe, and is traditionally thought to have been produced in supernova nucleosynthesis to seed the dust from which the Solar System formed. Because the Earth was molten when it was just formed, almost all of the gold present in the Earth sank into the planetary core. Therefore most of the gold that is present today in the Earth’s crust and mantle is thought to have been delivered to Earth later, by asteroid impacts during the late heavy bombardment, about 4 billion years ago.
Gold resists attacks by individual acids, but it can be dissolved by aqua regia (nitro-hydrochloric acid), so named because it dissolves gold into a soluble gold tetrachloride cation. Gold compounds also dissolve in alkaline solutions of cyanide, which have been used in mining. It dissolves in mercury, forming amalgam alloys; it is insoluble in nitric acid, which dissolves silver and base metals, a property that has long been used to confirm the presence of gold in items, giving rise to the term acid test.

Physical Properties

Cleavage: None
Color: Yellow, Pale yellow, Orange, Yellow white, Reddish white.
Density: 16 – 19.3, Average = 17.64
Diaphaneity: Opaque
Fracture: Hackly – Jagged, torn surfaces, (e.g. fractured metals).
Hardness: 2.5-3 – Finger Nail-Calcite
Luminescence: Non-fluorescent.
Luster: Metallic
Magnetism: Nonmagnetic
Streak: yellow

Photos :

Gold Colorado Quartz Mine, Colorado, Whitlock District, Mariposa Co., California, USA Size: 1.5 x 1.2 x 1.0 cm (thumbnail) © danweinrich
Leaf Gold Locality: Little Johnnie Mine (Ibex Mine), Leadville, Lake County, Colorado Specimen Size: 1.1 x 0.6 x 0.1 cm (thumbnail) © Mineral Classics
Eagle’s Nest Mine (Mystery Wind Mine), Placer Co., California, USA © Dona leicht
Gold Abrudbanya, Alba Co., Romania Size: 10.0 x 8.0 x 3.0 cm (cabinet) © danweinrich
Gold 9.2×6.0x4.5 cm Hollinger Mine Timmins Ontario, Canada This pure-white fragment of quartz has many rich patches of visible gold in it. Displays well. Copyright © David K. Joyce Minerals
These examples of natural gold nuggets are on display at the Smithsonian Museum of Natural History. The two samples are from Whitehall mine, Spotsylvania County, Virginia. The bottom sample is about 12 cm long.
This example of natural gold is on display at the Smithsonian Museum of Natural History. This massive gold sample is from Union Placer mine, California. Its mass is 2544 grams and it is about 25 cm long.
These examples of natural gold nuggets are on display at the Smithsonian Museum of Natural History. These are all samples of gold from Grass Valley district, Nevada County, California. The largest sample at the bottom is about 12 cm across and all samples are displayed at the same scale.
These examples of natural gold nuggets are on display at the Smithsonian Museum of Natural History. These samples are from Placer County, California. The largest is about 9 cm tall.
This example of natural gold is on display at the Smithsonian Museum of Natural History. Gold with quartz from California. The sample is about 8 x 10 cm.

Tourmaline Locality: Minas Gerais, Brazil

Tourmaline 
Locality: Minas Gerais, Brazil
Size: 3.8 x 1.3 x 1.1 cm
...
Turmalina

Localidade: Minas Gerais, Brasil
Tamanho: 3.8 x 1.3 x 1.1 cm

Foto Copyright © Di Anton Watzl

Geology Page
www.geologypage.com

Scientists make new discovery about bird evolution

Scientists make new discovery about bird evolution


Photograph of Eoconfuciusornis indet
In a new paper published in National Science Review, a team of scientists from the Institute of Vertebrate Paleontology and Paleoanthropology, the Shandong Tianyu Museum of Nature, and the Nanjing Institute of Geology and Paleontology (all in China) described the most exceptionally preserved fossil bird discovered to date.
The new specimen from the rich Early Cretaceous Jehol Biota (approximately 131 to 120 million years old) is referred to as Eoconfuciusornis, the oldest and most primitive member of the Confuciusornithiformes, a group of early birds characterized by the first occurrence of an avian beak. Its younger relative Confuciusornis is known from thousands of specimens but this is only the second specimen of Eoconfuciusornis found. This species comes only from the 130.7 Ma Huajiying Formation deposits in Hebei, which preserves the second oldest known fossil birds. Birds from this layer are very rare.
This new specimen of Eoconfuciusornis, housed in the Shandong Tianyu Museum of Nature, in Eastern China, is a female. The ovary reveals developing yolks that vary in size, similar to living birds. This suggests that confuciusornithiforms evolved a period of rapid yolk deposition prior to egg-laying (crocodilians, which are archosaurs like birds, deposit yolks slowly in all eggs for months with no period of rapid yolk formation), which is indicative of complex energetic profiles similar to those observed in birds.
This means Eoconfuciusornis and its kin, like living birds, was able to cope with extremely high metabolic demands during early growth and reproduction (whereas energetic demands in crocodiles are even, lacking complexity). In contrast, other Cretaceous birds including the more advanced group the Enantiornithes appear to have lower metabolic rates and have required less energy similar to crocodilians and non-avian dinosaurs (their developing yolks show little size disparity indicating no strong peak in energy associated with reproduction, and much simpler energetic profiles, limited by simpler physiologies).
Traces of skin indicate that the wing was supplemented by flaps of skin called patagia. Living birds have numerous wing patagia that help the bird to fly. This fossil helps show how bird wings evolved. The propatagium (the flap of skin that connects the shoulder and wrist) and postpatagium (the flap of skin that extends off the back of the hand and ulna) evolved before the alular patagium (the flap of skin connecting the first digit to the rest of the hand), which is absent in Eoconfuciusornis. Even more unique is the preservation of the internal structure of the propatagium which reveal a collagenous network identical to that in living birds. This internal network gives the skin flap its shape, allowing it to generate aerodynamic lift and aid the bird in flight.
The nearly complete plumage preserves remnants of the original plumage pattern, revealing the presence of spots on the wings and the earliest documentation of sexual differences in plumage within birds. This new specimen suggests that female Eoconfuciusornis were smaller than males and lacked tail feathers, similar to many sexually dimorphic living birds and the younger Confuciusornis in which the plumage of the males and females are different from each other. Samples of the feathers viewed under a microscope reveal differences in color characteristics, allowing scientists to reconstruct the plumage. Female Eoconfuciusornis had black spotted wings and gray body with a red throat patch.
Researchers have not found fossils from any other bird from the Jehol period that reveal so many types of soft tissue (feathers, skin, collagen, ovarian follicles). These remains allow researchers to create the most accurate reconstruction of a primitive early bird (or dinosaur) to date. This information provides better understanding of flight function in the primitive confuciusornithiforms and of the evolution of advanced flight features within birds.
“This new fossil is incredible,” said co-author Dr. Jingmai O’Connor. “With the amount of information we can glean from this specimen we can really bring this ancient species to life. We can understand how it grew, flew, reproduced, and what it looked like. Fossils like this one from the Jehol Biota continue to revolutionize our understanding of early birds.”

Qual foi a maior pedra preciosa já encontrada?


Qual foi a maior pedra preciosa já encontrada?

A recordista é de outro planeta

Superinteressante.com
A estrela anã branca Lucy – referência à canção “Lucy in the Sky with Diamonds”, dos Beatles – pode ser considerada o maior diamante do Universo. Descoberta em 2004, ela tem volume parecido ao da Terra e fica a 50 anos-luz daqui, na constelação de Centauro.
Uma anã branca é o que restou do núcleo quente de uma estrela após queimar todo o seu combustível – ainda demora uns 5 bilhões de anos, mas o Sol vai chegar lá. Cerca de 2 bilhões de anos após a morte do núcleo, composto basicamente de carbono, ele cristaliza e vira diamante.
Pulsações sonoras emitidas por esse tipo de estrela permitiram que os cientistas mapeassem o interior com tecnologia parecida com a dos sismógrafos usados para mapear as camadas geológicas da Terra.

As maiores pedras preciosas do planeta Terra

Diamante
Golden Jubilee: 109 g
Esmeralda
Gift from heaven: 536 kg (pedra bruta)
Safira
Millennium: 16,1 kg