The Wilderness of Bisti Badlands

The Bisti Badlands, which is also called Bisti/De-Na-Zin Wilderness, is a massive rolling landscape of phantasmagoric formations of earth and stone situated in northwestern New Mexico’s high desert lands. Bisti is resulting from the Navajo word “Bistahi” which means "among the adobe formations." De-Na-Zin takes its name from another Navajo word for "cranes." In this beautiful landscape here wind and water erosion over a long time have carved a imaginary world of bizarre rock formations and hoodoos in the form of pinnacles, spires, mushrooms and other rare forms that have fascinated names such as "Cracked Eggs", “Bisti Wings” and "Rock Garden".

This is untouched area so far and very least visited and mostly unknown was once an ancient riverine delta on the shores of an ancient sea, somewhere 70 million years ago. As the time passes the water gradually receded, lush foliage grew along the numerous riverbanks and several prehistoric animals wandered the area. Therefore, when the water disappeared completely, it left behind layers of jumbled sandstone, shale, mudstone, and coal. However, abundance of the coal burned away in ancient fires that lasted centuries. Moreover, erosion then formed the characteristic features of the contemporary landscape of the Bisti Wilderness. Furthermore 6,000 years ago, when the last ice age retreated, the waters of the melting glaciers assisted uncover fossils and petrified wood, as well as eroding the rock into the hoodoos now observable. Mostly three kinds of formations are bare in Bisti Wilderness area — the Ojo Alamo Formation, which has left naked the thick deposit of volcanic ash from an ancient eruption, and Fruitland formation and the Kirtland Shale. Here are recreational activities in the Bisti/De-Na-Zin Wilderness includes hiking, camping, wildlife viewing, photography, and horseback riding. Make sure, campfires are forbidden in the Wilderness.

The Ojo Alamo Formation extents the Mesozoic/Cenozoic boundary, and typically contains dinosaur remnants. Thus, the Fruitland Formation comprises layers of sandstone, coal and shale was laid down when the surroundings were marshy, humid and warm, with meagre drainage. The Fruitland Formation is found mainly on the western side of the Wilderness. However, the Kirtland Shale is the product of alluvial muds and overbank sand deposits from the numerous channels draining the coastal plain in the late Cretaceous period. Though, it overlies the Fruitland Formation, and is exposed on the eastern side of the badlands. Several of the gray hoodoos in the wilderness are made up of this formation. The exclusive egg-shaped formation, in the “egg factory” area, is also the result of erosion. Consequently, the cracks are the result of differential weathering conditions, whereas the speckled appearance due to mineral deposits in the stream that cut through the sedimentary rock. The Bisti Badlands is an amazingly scenic and colorful expanse of undulating mounds and unusual eroded rocks covering 45,000 acres, hidden away in the high desert even less publicized. The badlands are administered by the BLM (Bureau of Land Management), are free to enter, and are known officially, but less evocatively as the Bisti Wilderness Area.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Big Stone River, Russia

The “Big Stone River” is a chaotic jumble of massive boulders flowing down the slope of the Taganay Mountains in the Southern Urals, on the territory of Chelyabinsk Oblast, Russia. The big river of stone is 6 kilometers long and averages 200 meters in width and 700 meters wide. The enormous rock slide is thought to have formed during the last glaciation more than 10,000 years ago. Therefore, at that time, glaciers were well covered the top of the ridges of the Taganay mountains reaching almost heights up to 4,800 meters. Hence, under the gigantic weight of this ice, the top of the mountain was pulverized into masses of large boulders. Moreover, when the ice melted away, these rocks slowly slide down the hill making the Big Stone River. The geological feature is named “river” only because it look like as such, not because it really flows. Though, the rock slide has been sitting motionless for thousands of years, as the river is occupied by big blocks of quartzite an extremely compact and hard rock consisting of quartz including aventurine. This is a form of quartz containing mica or iron compounds that provides it a shimmering or glistening effect, weighing up to 9 to 10 tons each. The layer of rocks goes down 6 meters deep.

More interestingly, as one reaching the Big Stone River, the crisp sound of running water can be heard. The sound is created by small streams running under the rocks. Therefore, the Big Stone River is not the only stone river on earth though. Alike rivers of stone are found in other regions of the Ural Mountains. Outside of Russia, numerous stone rivers can be found in the Vitosha Mountain, in Bulgaria. One of the largest extends over 2 km in length is located on the Subalpine plateaus at the Zlatnite Mostove (‘Golden Bridges’) site in the upper course of Vladayska River. One more stone river in Vitoshka Bistritsa River valley is up to 300 m wide, and other stone run formations sprawl even wider on the mountain slopes.

The Saalfeld Fairy Grottoes, The Nature Best Piece on Earth

This is most enchanting place on earth, as there is no painter in the world as talented and skilled as nature, the magnificent burst of colors in these underground caves is maybe one of nature’s best pieces. The Saalfeld Fairy Grottoes are caverns or grottoes of a former mine near Saalfeld, in the German state of Thuringia. The Saalfeld Fairy Grottoes are famous for their myriad colorful mineral formations formed quite a lot of years by water dripping via soft rock. It is considered most colorful cave grottoes in the world. This Saalfeld Fairy Grottoes draws an average of more than 160,000 visitors annually. On 22 December 1913, scientists discovered the most beautiful part of the Saalfeld Fairy Grottoes, namely the Fairytale Dome stands with its awe-inspiring, sublime, illustrious in untouched purity and glory," writes Hermann Meyer, one of the discoverers.

The caverns comprise of three chambers connected by galleries. The first chamber presented the history of the alum shale mine opened for sightseeing in 1914. Historically, alum slate was used in a range of medicinal products, as a food preservative and in clarifying water. The historical background of this chamber about environmental radiation treatments formerly offered there until such treatments were found to be hazardous. The 2^nd chamber is the source of mineral laden water formed colorful stalagmites, stalactites and other shapes more than the centuries. However, 3^rd chamber comprises the famed “Fairy Kingdom” featuring a variegated grouping of deposits that, illuminated by theatrical lights and reflected in a perfectly still pool of water, is thought to resemble miniature castles and other buildings. It is known as “Feengrotten” in German, are in the Guinness Book of Records as the world’s most colourful cave, the most popular tourist attractions in the Thuringia, serve as a striking reminder of medieval mining.

The underground tour is breathtaking, reveals fascinating insights, the minerals they contains and thelives and labour of miners. There's so much to see, including a mineral magnifier, treasures of the mountain and giant scorpions. You can also grow your own stalactites and set molecules in motion, or piece together the minerals of the fairy grottoes and trace 440 million years of history in the panorama grotto cinema. This is a place of discovery for visitors young and old!

 

 

 

 

 

 

 

The Waffle Rock: A big attraction at Jennings Randolph Lake.

A large piece of rock is display in just outside the visitor center of Jennings Randolph Lake, in Mineral County, in the US state of West Virginia. The one side of the rock appears a usual waffle-like geometric pattern of raised, darker stone that runs in almost completely straight lines across the rock’s surface. The lines cross themselves at different angles forming deep pockets of lighter colored material. This strange formation has caused many to speculate on what might have caused such a strange pattern. The boulder lodged into the ground at Jennings Randolph Lake is a small piece of this rock that is believed to have broken off from the parent outcrop somewhere higher up the slope. A smaller piece of the same rock is also on display in the Smithsonian Institute of Natural History located in Washington, DC.

The bizarre patterning on the so-called “Waffle Rock” is a result of natural erosion, though over the years several alternative theories regarding its origins have evolved, and these engross pretty much the usual aliens, enormous reptiles and ancient Indian societies. The U.S. Corps of Engineers propose some insight into the rock’s formation.  The sandstone layers that make up the rock were formerly deposited about 250 to 300 million years ago. Then as the continent started to breakup by tectonic plate shifts, about 200 million years ago, the sandstone block was folded onto itself frequently creating cracks in the sandstone. Therefore, another 100 million years, the cracks started to fill with iron oxide, leached from the surrounding rock by the percolating water.

However, this iron oxide mixed with the sand grains in the cracks and formed a super hard material resistant to weathering compared to the surrounding sandstone pieces. Hence, the sandstone rock eroded away, it left behind the hard iron-oxide waffle like pattern on the rock. Moreover, the Waffle Rock formation is not regular, although alike patterned boulder have been found in Monongahela, Pennsylvania, and at Tea Creek Mountain in Pocahontas County, West Virginia. Numerous other undocumented examples of this stone patterning are in quite a few other places around the world. Still there’re so many peoples who refuse to accept that the Waffle Rock is a natural formation.  Hell, there are still people who think the Earth is flat perhaps we should bow to his superior knowledge on the subject. Now standing as an attraction for the public to view in person, the Waffle Rock boulder of West Virginia continues to draw the crowds to this truly ancient artifact. 

The Bungle Bungle Rane in Australia

The Bungle Bungle Range, in Purnululu National Park, is one of the most attractive geological landmarks in Western Australia. The Bungle Bungle range features unique beehive-shaped sandstone towers and conglomerates alternately striped in black and orange bands. The Bungle Bungle Range formation occupies an area of nearly 450 square kilometers. The Bungle Bungle Range is a spectacularly incised landscape was not really discovered as a travel destination until the mid-1800s. The researchers believed that the sedimentary rocks of Bungle Bungle were formed in the Ord Basin 350 million years ago, when active faults were altering the landscape. The stunning rocks rises up to 578 metres above sea level, and stand 200 to 300 metres above a woodland and grass-covered plain, with steep cliffs on the western face. If you’re flying over Bungle Bungle range, it is a striking sight. Moreover, the area was traditionally occupied by Karjaganujaru peoples; they’re living here for more than 20,000 years, having strong affiliation to this ancient landscape.

The joint effects of wind from the Tanami Desert and rainfall over millions of years shaped the domes. Although the formation appears solid, the sandstone is very brittle. The weight of overlying rock holds the sand grains in place, but when this is removed, the sandstones are without difficulty eroded. The rounded tops imitate this lack of internal strength. Moreover, the water flowing over the surface will exploit the softness and irregularities in the rock, such as cracks or joints, and swiftly erodes the narrow channels that separate the towers. Cyanobacteria can't grow here and without the protective coat the surface is exposed to "rusting". Thus, one of the most prominent features of the sandstones is the alternating black and orange or grey banding. However, the darker bands comprises of permeable layers of rock, which let water to move through with ease. As the water keeps the rock surface moist letting dark algae to grow on them. Hence, the less permeable layers in between are well covered with a patina of iron and manganese staining, producing the orange bands. These outer coatings support to keep the lower parts of the towers from erosion.

Furthermore, a 7 km diameter circular topographic feature is clearly visible on satellite images of the Bungle Bungle Range. It is supposed that this feature is the eroded leftover of a very early meteorite impact crater that maybe hit the area somewhere 250 million years ago. This beautiful structure is well known as the Piccaninny impact crater. The range remained largely unidentified except by local Aborigines and stockmen until 1982 when film-makers arrived in this area and produced a documentary about the Kimberley. The area was gazetted as a National Park in 1987 and was also inscribed as a World Heritage area in 2003.