In 1867, in a field in Denmark, a little boy discovered something magical. Hindsgavl Dagger is Hindsgavldolken

It was immediately brought to the property managers attention. He offered the boy the equivelant of 90 dollars, and he couldn’t refuse. The manager then gifted it to the owner of the estate.  Basse Fonss of Hinsgavl Manor.

Hingsgavl manor was apart of the Hindsgavl. It’s the pieces of land that connect Frederica and Middlefart (centre of Denmark).

As the Exposition Universelle at Paris approached in 1889. Danish collectors realized they needed something big. The museum never lent out objects but always sent copies.  Since Hindsgavldolken was private owned, Basse Fonss was approached. He agreed to lend it out. 


After the Exposition universelle, the museum and collectors were so impressed with its attraction and features. They made Basse an offer he couldn’t refuse.   

About:
Production of stone daggers continued into the bronze age. Especially in the north. It’s believed this dagger was produced around 4000 years ago. It is almost 30cm long, and the blade thickness is less than 1cm. It shines a beautiful black and brown.

Did you know? The 100 krone danish bank note (about 15.5$ usd) features Hindsgavldolken, or Hindsgavl Dagger.

Font-de-Gaume is a well known cave in south west France

Located near Les Eyzies-de-Tayac-Sireuil in the Dordogne department.
Font-de-Gaume cave contents contain paintings in several colours dating to almost 30,000 years.

While exploring the area, in 1901 Denis Peyrony discovered the paintings.

Prehistoric people lived in the Dordogne valley around 25000 thousand years ago. The cave was inhabited for several thousand years. Something must have happened. Because there after, the cave is believed to be long forgotten.

Many of the drawings date from around 19,000 years ago. The most famous is of 5 bison, and was discovered by accident in the 1960s when scientists were cleaning the cave.
More than 230 figures are believed to have been recorded in the cave. Included is 80 bison, 40 horses and 20 mammoths. Some say there are even more yet to be discovered.

Did you know? 200 of the paintings are in multi colour. Making Font-de-Gaume one of the best examples of polychrome (multi colour) paintings other than Lascaux.

Check it out today.

Cap Blanc rock shelter is a limestone rock shelter with sculptures, and magdalenian women. It is in the west of France.

In 1908 Cap Blanc was discovered under supervision, while others worked nearby uncovering Lascaux and the Lascaux cave. While digging they found one of the most impressive carvings from the upper paleolithic.
Following the uncovering of this, the carving and additional frieze, in 1911, they built protective walls around the area. It included lowering the floor. And, at which point one of the workers hit a skull. It was Magdalenian women.

Located in the Marquay commune on the right bank of the Beune River, a few kilometers west of Eyzies-de-Tayac, in Dordogne.

What is a frieze? A frieze is a broad horizontal band of sculpted or painted decoration, especially on a wall near the ceiling.

The frieze depicts a number of animals, some in haut-relief, dating back 15,000 years. These include ten horses (one measuring 2.20 m long), at least three bison, ibex and several incomplete figures. The sculpted frieze occupies 13 of the 16 meters of the shelter.
Some of the carving are as much as 30 cm deep. Red ochre covers much of the frieze and some of the area around it is now difficult to see. Among other flint tools probably used to create the frieze were found with the Magdalenian women and include burins and scrapers.

The skeleton known as Magdalenian women is that of an early modern human dating from 13,000 to 11,000 BCE, during the Magdalenian period. It is the most complete upper paleolithic skeleton in northern Europe. When Magdalenian women was acquired in 1926 for the Field Museum in Chicago, Illinois, by Henry Field, then curator of Physical Anthropology. It was hailed as one of the most significant acquisitions the large museum ever made. On the first day the precious skeleton was exhibited, tens of thousands of visitors flocked to the museum to see it.

In 1910 the site was classified as a French historical monument. Currently there are guided tours, a museum and replica of magdelenian women. Be sure to check it out!

In the environment surrounding Eyzies-de-Tayac Sireuil village. Lascaux is located some distance from the major concentrations of decorated caves and inhabited sites. With cave drawings estimated to 16 or 17 thousand years.

The area has no fewer than 37 decorated caves and shelters, as well as an even greater number of habitation sites from the upper paleolithic (cave man) era. These sites are the highest concentration in Europe.
Geologically, the Vézère drainage basin covers one fourth of the département of the Dordogne (river). At its centre point, the river’s course is marked by a series of turns flanked by high limestone cliffs.

The entrance to the Lascaux Cave was discovered by 18-year-old Marcel Ravidat when his dog, Robot, fell in a hole, in 1940. It was getting late in the year, and in an dangerous area, so he decided to return with some friends another day. They entered carefully through a 15m or 50 feet shaft. The teenagers discovered that the cave walls were covered with depictions of animals. Some dating to an estimated 17,000 years.

6,000 figures: animals, human figures, and abstract signs, in about 600 areas were found.
Using mineral pigments, red, yellow, and black colours were crushed and mixed from a complex multiplicity of plants and minerals. Included was iron compounds such as iron oxide (ochre), hematite, and goethite, As well as manganese-containing pigments. These were a little more advanced than taking charcoal from a stick and drawing on the wall. Many of the images are now precisely studied. 364 paintings are horses, as well as 90 paintings of horned deer. Also represented are cattle and bison, each representing 4 to 5% of the images. There are a bunch of other unique images, includes seven felines, a bird, a bear, a rhinoceros, and a human.

The most famous section of the cave is the Hall of the Bulls where bulls, equines, aurochs, stags, and even a cave bear is depicted. One of the 36 animals represented here is a bull. It is 5.2 metres (17 ft 1 in) long. The largest animal discovered so far in cave art. And, some of the bulls in this drawing appear to be in motion.
On some of the other cave walls, unique art methods were used. It is believed colour was applied as a suspension of pigment in either animal fat or calcium-rich cave groundwater or clay, and applied using swabbed or blotted paint, instead of brush. In a few other areas, the colour was applied by spraying the pigments by blowing the mixture through a tube. Many images are faint or totally deteriorated. Where the rock surface is softer, some designs were incised into the stone.

Did you know? After the cave had been opened, 15 years later, by 1955, carbon dioxide, heat, humidity, and other contaminants produced by 1,200 visitors per day had visibly damaged the paintings. As air condition deteriorated, fungi and lichen increasingly infested the walls. Consequently, the cave was closed to the public in 1963, and instead, it was decided 4 replicas get created nearby the cave site.

History of log cabin building

Log cabins have been affiliated with almost anything living. However more often than not, it has been the ancient history in Europe and the early settlers in the eastern US and Canadian wilderness. When do you think humans started log cabin building?
In Northern Europe or Russia, there are cabins from 3 or 4 thousand years ago. Ones that had there roofs somewhat maintained are still standing, or have been up cycled elsewhere.


Similarly to the lack of raft, ship and boat evidence before 1500ad. During roman, and war times, it was noted many log cabins were built, to be de-constructed and transported to battlefields, for weapons; even boats, jigs, firewood or whatever manufactured wood pieces were necessary at the time. It’s believed not much was left around but was re-used sustainably.
Most cultures were log cabin builders. Provided they had a flint, chert or sharp enough lithic tool supply. To manufacture broadaxes, and other pieces of stone capable of chopping suitable flat trees down, and notching the bark and tree part way out to overlap.

Architecturally speaking, in De Architectura, was the first mention of log cabins using construction with logs. It was described by Roman architect Vitruvius Pollio (20-30bc). He noted that dwellings in northeastern Turkey were constructed by laying logs horizontally overtop of each other and filling in the gaps with “chips and mud”. Most people nowadays call it chinking.

In modern times, important aspects of log cabin building are often the site upon which the cabin was built. It is aimed at providing the cabin inhabitants with both sunlight, drainage, and protection from wind and rain to help them able them see better. And, to be able to thrive and cope. Finding trees in an area on or nearby your building site, is an important factor, and thus studied in archaelogical and building site history because of it (even though most of the logs are decomposed). Extreme weather, animal attacks, and staying warm; dry and safe are also factors.

Did you know? Log cabins have origins in US politics since the early 19th century. At least seven United States presidents were born in log cabins, including Andrew Jackson, James K. Polk, Millard Fillmore, Franklin Pierce, James Buchanan, Abraham Lincoln, and James A. Garfield. William Henry Harrison was not one of the presidents. However during the 1840 presidential election his party were the first to use a log cabin as symbol to show Americans that he was a man of the people.

Did you know? Possibly the oldest surviving log house in the United States is the C. A. Nothnagle Log House (c. 1640) in New Jersey.

More recently coastal and interior log cabins builders have become popular due to there proximity to large fir, cedar, spruce and pine trees. And, the sustainability aspects of building close to the forest.

Interested in log cabin building?
Contact us/create account today.

References:
Revised Log Construction Manual – Ultimate Guide To Building Log Homes – Full Color Edition Paperback – Unabridged, January 1, 2016
by Robert W. Chambers (Author) ISBN-10 ‏ : ‎ 0971573638

Wikipedia: https://en.wikipedia.org/wiki/Log_cabin

Плейстоценовый парк, or Pleistocene Park. In NE Siberia an attempt to re-create subarctic steppe grasses to help reduce greenhouse gases, climate change & a better more significant world is taking place.

Family members Sergey Zimov, and Nikita Zimov are testing a big hypothesis. Repopulating with large herbivores (and predators) can restore rich grasslands ecosystems. And, that if overhunting, and not climate change was primarily responsible for the pleistocene epoch, quanternary, or big event 11,700 years ago.

Another main aim, is to research the changes expected by the climatic effects of restoring the 10,000 year old plus ecosystem. The hypothesis is that change from tundra to grassland will result in a raised ratio of energy emission to energy absorption of the area, leading to less thawing of permafrost, and thereby less emission of greenhouse gases. It is also thought that stomping and the removal of snow by large herbivores will reduce permafrost insulation sucking in the pollution, even in cold winter.

Melted permafrost is changing the planet:
Greenhouse gasses are warming the planet. Some areas, like Siberia (Russia has 11 of the 18 million square km of permafrost), it is observed more than others. But believe it or not. When there is a lot of snow, the ground and the permafrost do not get much colder in winter. Its why its called permafrost. When these soils thaw though, old microorganisms wake up and attack. What they have not had time to consume. Releasing carbon dioxide when the soil is dry, and methane when it is saturated with water. Due to climate change, it doesn’t help because this area, it is experiencing more rain.
From the melting of the permafrost, if it was only co2 released, rather than both co2 and methane. The emissions is equivalent to that of human beings. For the greenhouse effect (and thus melting of the permafrost) methane gas can be 4 times worse than carbon dioxide. Resulting in even greater global warming. It is a big paradox. Many people do not understand this. The methane released from permafrost is more dangerous than carbon dioxide and both are bad.
In the grassland ecosystem, everything that grew during the summer must be consumed in the winter. Large herbivores need to eat. The only way to access the grass during the cold season is to dig through the cold snow. The parks animals dig in the snow all winter long. This contributes greatly to the cooling of the soil. And, absorption and release of the greenhouse gases.
It was observed that many greenhouse gases decreased during the first year and a half of covid19. While things were shut down. Instead of decreasing the methane gases increased. Due the permafrost melting. Regularly observed were appearances of new small springs where methane gases were bubbling up, in areas that used to be snow and permafrost. Other than the permafrost melting, and being replaced by trees shurbs and mosses. Not grasses, which prehistoric herbivores eat up, and stomp down. Many cannot see any other explanation for preventing this high concentration. The theory purposes that restoring the wildlife and ecosystem will absorb more greenhouse gases and help restore our natural environment. Sergey has been quoting telling the UN: “I created Pleistocene Park to observe how quickly animals could transform the moss tundra into productive grassland… why had the natural environment, which had known so many grasslands, horses, bison, mammoths, become so poor?” Permafrost has long been treated like an unwanted child in the scientific family. Reports are that by 2100 we will have lost another 10-20 percent. It is a big controversial topic.

Goals:
Researching the effects of large herbivores on the arctic tundra/grasslands ecosystem, and preserving the environment; and,
To research the climatic effects of the expected changes in the ecosystem. Here the key concept is that some of the effects of the large herbivores, such as eradicating trees and shrubs or trampling snow, will result in a stronger cooling of the ground in the winter, leading to less thawing of permafrost during summer and thereby less emission of greenhouse gases.

Sergei Zimov points out contradiction to this scenario:
Similar climatic shifts occurred in previous interglacial periods without causing such massive environmental changes as we are seeing today;
Those large herbivores of the former steppe that survived until today (e.g. musk oxen, bison, horses) thrive in humid environments just as well as in arid ones; and,
The climate (both temperatures and humidity) in today’s northern Siberia is in fact most similar to that of the mammoth steppe.

Did you know? Permafrost is a large global carbon reservoir that has remained frozen throughout much of the Holocene. It is ground that continuously remains below 0 °C (32 °F) for two or more years. It is not necessarily under the snow too. Sometimes it is found hundreds of meteres deep. Due to the recent climate changes, the permafrost is increasingly thawing, releasing stored carbon and forming thermokarst lakes. When the thawed permafrost enters the thermokarst lakes, its carbon is converted into carbon dioxide and methane and released into the atmosphere. Methane is a potent greenhouse gas and the methane emissions from thermokarst lakes have the potential to initiate a positive feedback cycle. In which increased atmospheric methane concentrations lead to amplified global climate change. Which keeps the ball rolling to more permafrost thaw, more methane and more carbon dioxide emissions. Included in the higher temperatures, rain and climate change you see in almost all places today.

Implementation & background: regional pleistocene ecoregions. Regenerate the pleistocene terrain with its different ecological habitats such as taiga, tundra, steppe and alpine terrain:
Mainly recreate the extensive grasslands that covered the Beringia region in the late pleistocene. Mammoth steppe with large and medium herbivores. Species woolly mammoth, woolly rhino, steppe wisent, lena Horse, muskox, and reindeer. Saiga antelope, some massive herds. On the edges, barrier shrub-like terrain, and dry conifer forests (similar to taiga): woolly rhinoceros, moose, wapiti, yukon wild ass, and camels. Beyond this, mountains, more mountain-going animals like: snow sheep. Variety of carnivorous mammals. Like on the plains: beringian cave lion, apex predators, shared grey wolf, cave hyena, homotherium, brown bear, wolverine, and arctic fox. In shrubs and forests there were also brown bears, wolverines, cave bears, lynxes, tigers, leopards, and red foxes.

Did you know? Siberian tiger and Amur leopard occupied the southern present Russian-Sino border in the Amur and Primorye regions. And, both have been purposed for the park.

Proposed procedure:
Few of the former species of megafauna are left; and their population density is extremely low, too low to affect the environment. Desired results density raised artificially by fencing in and concentrating existing large herbivores. A large variety of species is important as each species concerns. For example are the effects on the flora (are the mosses being replaced by grasses, etc.), the effects on the atmosphere (changes in levels of methane, carbon dioxide, water vapor) and the effects on the permafrost.
Once a high density of herbivores over a vast area has been reached, predators larger than the wolves will have to be introduced to keep the megafauna in check.

Did you know? It is believed anywhere permafrost currently exsists, or even areas burned from forest fire, the mammoth steppe can be re-created. Reducing greenhouse gases. The rate of decomposition of organic matter in the soil where there were fires depends mainly on temperature. Introducing grasses and mammoth steepe slows the process down. The only way to force the soil to retain carbon is to cool it down. For a long time, scientists have known, that dark forests absorb the sun’s rays, while the lighter, snow-covered grasslands reflect them in winter. Having a combination can have positive effects on the permafrost and environment.

White spruce

Pleistocene progress:
-1988–1996: The first grazing experiments began in 1988 at the northeast science station in Chersky with yakutian horses.
-1996–2004: In 1996 a 50 ha (125 acre) enclosure was built in Pleistocene Park. As a first step in recreating the ancient landscape, the yakutian horses were introduced, as horses most abundant ungulates. Moose, already present in the region, introduced. The effects of larger animals (mammoths and buffalo) created by using a tank and 8×8 Argo to crush pathways through the willowshrub.

Willowshrub


Experiment working:
The vegetation in the park started to change. In the areas where the horses grazed, the soil compacted. Mosses, weeds and willow shrub were replaced by grass. Flat grassland is now the dominating landscape inside the park. When air temperature sank to −40 °C (−40 °F) in winter, the temperature of the ground was found to be only –5 °C (+23 °F) under an intact cover of snow, but −30 °C (−22 °F) where the animals had trampled down the snow. The grazers thus help keep permafrost intact, thereby lessening the amount of methane released by the tundra.
-2004–2011: A new fence was erected. After complete, reindeer and more moose were brought into the park.
A 32 meter (105 foot) high tower was erected in the park, in 2007, that constantly monitors the levels of methane, carbon dioxide and water vapor in the park’s atmosphere.
Muskox from Wrangel island were reintroduced in 2010
In 2011, Altai wapiti were introduced
-2011–2016: Construction of a new branch begun on the “Wild field section”, and greater energy monitoring stations were put in.
-2017–present: yak, and sheep were brought to the park. More plans for future.

Reception & Controversial aspects:
Critics admonish that introducing alien species could damage the fragile ecosystem of the existing tundra. Scientist Sergey Zimov replies: “Tundra – that is not an ecosystem. Such systems had not existed on the planet [before the disappearance of the megafauna], and there is nothing to cherish in the tundra. Of course, it would be silly to create a desert instead of the tundra, but if the same site would evolve into a steppe, then it certainly would improve the environment. If deer, foxes, bovines were more abundant, nature would only benefit from this. And people too. However, the danger still exists, of course, you have to be very careful. If it is a revival of the steppes, then, for example, small animals are really dangerous to release without control. As for large herbivores – no danger, as they are very easy to remove again.”
Another concern point is a majority of species cant be introduced in harsh conditions. For example, according to some critics, the yakutian horses, would not survive without food supply and human intervention. Mostly in the fall when water freezes and before the snow hits (the horses eat the snow for water, but cant lick the ice as easily).

Positive reception:
Project drawdown claims the park as: “100 most substantive solutions to global warming”. Total costs and lifetime savings were monitored in the study.
In January 2020, a study from the University of Oxford assessed the viability of the park’s goals. It was estimated, if three large-scale experimental were set up, each containing 1000 animals. Over a ten year period, that 72,000 metric tons of carbon could be held and generate 360,000 US dollars in carbon revenues.

Visitors:
The park is a select hub for a small number of journalists; and, international scientists, and students, who come from around the world to conduct their own ecological research and experiments.

Size and administration:
Pleistocene Park is a 160 km square scientific nature reserve (Zakaznik) consisting of willow brush, grasslands, swamps, forests and a multitude of lakes.
The average temperature in January is about –33 °C; and, in July +12 °C; annual precipitation is 200–250 mm.
The reserve is surrounded by a 600 km 2 buffer zone.

Animals:
Herbivores: Reindeer (Rangifer tarandus);
Elk;
Moose (Alces alces);
Yakutian horses;
Muskox (Ovibos moschatus); and
European bison, Bison bonasus).

Muskoxen family: Domestic yak (Bos mutus grunniens);
Edilbaevskaya sheep (a domestic breed of sheep);
Kalmykian cattle (a domestic breed of cattle adapted for the Mongolian steppe);
Plains bison (Bison bison bison);
Orenburg fur goat (Capra aegagrus hircus); and,
Bactrian camel (Camelus bactrianus).

Carnivores: Eurasian lynx (Lynx lynx);
Tundra wolf (Canis lupus albus);
Arctic fox (Vulpes lagopus);
Eurasian brown bear (Ursus arctos arctos);
Wolverine (Gulo gulo);
Red fox (Vulpes vulpes);
Sable (Martes zibellina); and,
Stoat (Mustela erminea).

Herbivores considered for reintroduction:
Wood bison (Bison bison athabascae);
Bison priscus;
Altai wapiti or Altai maral (Cervus canadensis sibiricus);
Wild yak (Bos mutus);
Snow sheep (Ovis nivicola);
Wild Bactrian camel (Camelus ferus);
Siberian roe deer (Capreolus pygargus);
Saiga antelope (Saiga tatarica); and,
Altai maral.

Carnivores:
Siberian tiger (Panthera tigris tigris).

Did you know? Harvard universities geneticist George Church, and others are working on a plan to genetically resurrect woolly mammoths.

Animals that could be placed in the park if revived from extinction:
Woolly mammoth (Mammuthus primigenius);
Cave lion (Panthera spelaea);
Steppe bison (Bison priscus);
Woolly rhinoceros (Coelodonta antiquitatis);
Irish elk (Megaloceros giganteus); and,
Cave bear (Ursus spelaeus).

Slip into your own pleistocene freedom. Wander free and create your own natural time of life. Your kind will grow stronger and stronger, as the millennia go on and on and on. Earth may overflow with life one day again. Maybe one day, all of our mistakes may even be taken back. And if it does. And, if we save the planet and be ourselves, that will be the sh*t.

Cave of the Trois-Frères is a cave in southwestern France famous for its cave paintings from 13,000 years ago.

Recreation of some of the drawings. At a french museaum

It is located in Montesquieu-Avantès, in the Ariège département. Near the Spanish border. The cave is named for three brothers (French: trois frères), Max, Jacques, and Louis Begouën, who, along with their father Comte Henri Begouën, discovered it and the signigifance in 1914.

Big info:
One of the paintings, known as “The Sorcerer”, is the “most famous and enigmatic human figure” with the features of several different animals. Though given there age, each and exact characteristics remain a matter of debate. Conesyahoo had stated ‘it was an irish elk with a magicians head spitting something’.


Engravings were found in the cave and nearby included what is though to be the earliest representation of an insect. Also appeared were what appear to be several birds, and a cave cricket found on a fragments of a bison bone.
On the other walls are whats believed to be: lions, owls, and bison. A horse overlaid with club-like symbols, and an apparent speared brown bear vomiting blood.
Aside from the “Sorcerer”, other human-like figures can be seen at Trois-Frères, such as the man-bison, and a character known as the “small sorcerer” who appears to be playing a nose-flute.

Location:
The Trois-Freres cave is part of a single cave-complex formed by the Volp River. The complex is divided into three caves; the central Trois-Freres, Enlène to the east, and the Tuc d’Audoubert to the west. The river flows through some of the lower sections. With different galleries sectioned on each level and room.

Did you know: One area, the ‘salle des bisons’ contains two masterfully modeled bison, which were sculpted in clay with a stone spatula-like tool and the artist’s fingers. It is believed the pair are among the largest and finest surviving prehistoric sculptures.

Kapova Cave, known as Shul’gan’tash. A limestone karst cave in the southern Urnal mountains. It’s known for 16,000 year cave drawings.

Kapova cave (Капова пещера), Shul’gan-Tash ( капающая вода), dripping water, or Шүлгәнташ in Bashkir. It is a limestone karst cave in the Burzyansky District of Bashkortostan. About 200 km (120 mi) south-east of the city of Ufa, above Kazakhstan. It is in the southern Ural mountains.

In Bashkir tradition. Shulgan was mostly negatively attributed. To the owner of the underworld, or underwater king. Given the history and geology, both the lake and cave also bear part of his name. Bearing a significant part of Russian and the areas folklore and tradition.

Kapova cave entrance:
Today, this area of wild dense forest, and high white rocks has changed. It is the habitat of deer, bear, and bashkort bee. Around 10-20 thousand years ago the climate and the landscape was different. Summer was short, while winter months were very long and cold. Much of the landscape was Tundra. In the clefts and caves among the rocks humans huddled together to keep warm.
The entrance to the cave is situated on the southern slope of the Sarykuskan mountain. It forms a huge arch of 30 m (98 ft) height. To the left of the entrance to the cave is a lake from which the river Shul’gan originates. Inside the cave flows the underground Shul’gan river. That created the cave. This three-storey cave system is huge. Its about 3 km (1.9 mi) long, with a vertical amplitude of 165 m (541 ft) including siphon underwater cavities, large halls, galleries, underground lakes and the river.

The portal:
The mouth of the ‘Shulgantash cave’ is now called the portal. Deep in the portal the Shulgan stream comes up through the earth forming a pool named Blue lake. Its believed the lake is bottomless. Below 33 Meters (108ft) in depth it joins a gigantic underground water cavity.
A passageway leads from the portal to the succession of the ground level halls, and galleries. Some are as high and wide as 20-30 meters. The halls and galleries are connected by tunnels of various lengths and shapes. Some of the walls too are covered with calcite sinter. Which is quite deep and intricately shaped.
According to scientist P.I. Rychkov, Bashkirs (Bashkorts) usually hid here their famiIies, and horses during wars, and their uprisings. The cattle naturally stayed in the lower floor of the cave, while women, children and old men went upstairs. Food was always stored here.

Cave drawings:
These Russian cave drawings, discovered in the late 1950s were the first of there age, beyond France and Spain. And, unrivaled versus anywhere else on earth. For many centuries all the thousands of year old cave drawings here had been covered with a semi-transparent calcite crust. In 1976, a known archaeologist O.N. Bader was asked to begin cleaning some of the pictures off. Traces of primitive, human life, spread, red paint, as well as, ornament of geometrical figures. Neolithic signs (and, older) of human life are in the large cave system. Two-coloured pictures of long-haired horses, beside them a trapezium like geometrical figure, and a little further, a group of geometrical signs. There is a picture of an anthropoid creature, the only one in Shulgantash cave. Ancient people, various animals: horses, rhinos, bulls, bisons, and mammoths. Geometrical signs and figures. In all, there are many drawings in ‘Kapova, Shul’gan-Tash, dripping water or Шүлгәнташ cave’. Still being analyzed daily. Size varies from 44 to 112 centimeters. Uranium-thorium dating showed that the oldest drawings in the Kapova cave were made 36,400 years ago. That’s amazing.

Underground lake in the cave:
In one of the halls you can see the river Shulgan in its underground flow. A scuba diver traveled almost 330 meters (1082 feet or 1/3km) into a siphon inside the cave having finding no end to it. Due to the geology of the gave. Silvery fringe of calcite icicles hang from some of the ceilings. And, among the sublime decorations of the cave are “milky rivers” composed of there crystals. Fragile and crisp. They haven`t become solid like pearls yet. Adding discrepant beauty to the somewhat dark underworld place.
On some of the walls are crusts of marble onyx, in some places half a metre deep.

Did you know? Marble onyx has only been found in caves.

Discovery, excavation:
It had long been said, locals were afraid to visit or document about the cave. The first written information was in 1760. Initial Russian academy of sciences member, P.I. Rychkov gave a detailed description of the cave ground level in his article: “Description of a cave located in the Orenburg province near the Belaya River, which of all the caves in Bashkiria are the most glorious and revered”. From then on, other scientists, foresters and locals begain documenting and taking explorations into the cave. Even offering tours for explorers and those so inclined.
Beginning around the 1960s, employees of Bashkir state university begin compiling a real map of the cave. A number of years later, when some of the scientists died, and they decided to close the cave in 1979.
When re-opened in the 1980s, dating technology had also increased. Scientists were able to analyze the drawings greater. And, in addition, find a clay fat lamp; stone, mostly flint tools; pieces of ocher, jewelry in the form of beads; and, pendants made of stone and small shells of fossil mollusks. Bones of animals of the pleistocene: mammoth, cave bear, fox, hare, marmot were also found. Even pikas, and jerboa. Many large archaeologists agree Shulgan-Tash cave was a sanctuary and one of the most significant pieces of history in Russia. Check it out today.

Times of our lives 3?: 100$ pieces of plastic w/ copper, lithium and precious metals. Maybe we don’t know what fun is anymore

There was a time when we valued $100 pieces of plastic w/ copper and precious metals. Combined with disease, and vaccines, so corporations could amount mass data. A microchipped robotic digital future.

Yet we don’t know much past 5 or 6 thousand years. 30,000 years and beyond. Almost nothing. Who and what were these people? And, what constitutes a lively, or true “time of life” events?