Finally, the expected 28th Episode trailer came and we learned that Alparslan Great Seljuk will start on Monday, September 19th.
With the new trailer released, it contains many clues about the season. So what will happen in the new episode? Who is Aslan Yusuf that Alparslan fought?
Why is Alparslan sitting on Tugrul Bey’s throne? Who ruled Alparslan’s marriage to Seferiye Hatun? The answers to these questions are in our video. The new Tekfur of Ani, Gregor, is much more cunning than Kekavmenos.
He will try to slow down the Seljuk state by collaborating with Aslan Yusuf to keep Alparslan away from his own lands. Aslan Yusuf is an Emir of the Ghazni State.
Collaborating with Ani Tekfuru, he will make the Ghaznavids and Seljuks fight and try to rise from the middle. Meanwhile, we learned that Seferiye Hatun is the daughter of Emir Aslan Yusuf and came to take revenge on Alparslan.
In the note sent to Alparslan, it was decreed that he marry Seferiye Hatun, only the Caliph could make such a decision, and his aim is that the two Muslim states want to be allies with each other by establishing kinship relations.
But the new season will be very exciting with all kinds of events. The only logical explanation for Alparslan to sit on Tuğrul Bey’s throne and his father Çağrı Bey is still alive can be the only logical explanation.
Once a vast prehistoric sea, the Nullarbor Plain in South Australia is an extraordinary landscape. Now a rugged desert on limestone bedrock, it is extremely flat and almost featureless, stretching for over a thousand kilometres.
But a new discovery suggests the vast semi-arid expanse may not be as simple as we thought. Using satellite images, an international team of scientists led by geologist Matej Lipar from the Slovenian Academy of Sciences and Arts has discovered an ancient landform that appears to have once been a coral reef – or part of it.
Coral reef. Although we know that limestone can form from calcium carbonate from shells and fossils, and although Nullarbor Limestone is rich in fossils of corals and algae, there are no characteristics principal associated with carbonate accumulation.
The rock relief consists of a circular raised ring about 1,300 meters (4,265 ft) wide with a dome in the center, and may be the earliest primary deposit structure discovered in the field.
Unlike many parts of the world, much of the Nullarbor Plain has remained largely untouched by the processes of climate change and erosion over millions of years, making it a unique geological canvas recording history.
old – and definitely worth investigating if you have the right tools.Much of Australia is now dry and arid, with vast inland deserts. Millions of years ago, however, during the Miocene, the continent teemed with life; Not only dense and thriving forest ecosystems, but also huge inland seas.
The sea that covered the Nullarbor began to dry up about 14 million years ago, exposing shallow limestones that had been deposited in the Middle Cenozoic. Since that time, geologically, very little has happened on the ground.
There was no significant sediment deposition to speak of, nor major upheaval that led to the formation of mountain ranges or other features. This means that the Nullarbor is effectively a clean record of geological processes and features dating back to the Miocene.
“Evidence of long-extinct river channels, as well as sand dune systems directly imprinted in limestone, preserves records of ancient landscapes and even present-day winds,” says Brahms. “And it’s not just the scenery.
Isolated cave shafts scattered across the Nullarber Plain preserve the mummified remains of Tasmanian tigers and the complete skeletons of long-extinct wonders such as Thelaklio, the marsupial lion.” That’s not all.
“On the surface,” Brahms added, “due to relatively stable conditions, the Nullarbor field has preserved a large number of meteorites, giving us a glimpse in time of the origins of our solar system.”
It’s only with recent advances in high-resolution satellite imagery that scientists have been able to uncover some of the more subtle features of the field, including rock texture. Analysis of a few rocks
extracted from the limestone reveals fossilized benthic foraminifera, single-celled marine organisms.
This discovery is consistent with the Nullarber limestone. But one of the samples revealed something interesting: microbial bonding stone, a type of stone bonded to coral or algae when it formed.
No other microbial boundary stone has been identified in the Knullbar Limestone, and this organism is capable of depositing organic matter. Its presence suggests that the rock-like structure dates back to when the limestone was deposited.
