Bora-Bora holidays. French Polynesia sandy beaches. Tahiti black rocks sunny day landscape. Bora-Bora island tours

What could be nicer than a glass of juice after a long journey? Only fresh juice. Here you are greeted by breathtaking landscapes, clear ocean waters, neat bungalows near the water with a covered reed roof, interesting culture and rich history of the island. For a long time, the name Pearl of the Pacific Ocean stuck on the island of Bora Bora, and you involuntarily agree with this, barely seeing a turquoise lagoon surrounded by corals, magnificent white beaches, motu - small picturesque islands. It is located two hundred and thirty kilometers from the capital of French Polynesia - Papeete, located on the island of Tahiti.

The main part of the locals of the island of Bora Bora live along the coastal strip bordering the island. The atoll ring is open in the west, and even cruise liners can pass from the ocean into the lagoon through the Tiavanui navigable canal. The main city and port of Vaitape is located opposite this strait, next to the highest peak Otemanu. Mota taxi can take you to the beach with encyclopedic white sand. It will take you back to the hotel at the agreed time. There are excellent resorts not only on the main island but also on the motus islands surrounding the lagoon. The best hotels and beaches are located in two large bays in the south-west of the island, between Pointe Paoaoa and Pointe Matira. Matira Beach is the only public beach of the island, the rest are privately owned.

Lagunarium of the island of Bora Bora is one of two in all of Polynesia. It is located in the center of Bora Bora lagoon, near one of the best hotels on the island - Le Meridien Bora Bora. The second lagunarium is located on the island of Tahiti. It differs dramatically from traditional aquariums, because here you can take a pipe, a mask, and, jumping into the water, calmly swim among turtles, rays and other tropical fish.

Our planet formed about 4.54 billion years ago in the process of dust accretion and sintering of tiny viscous droplets of matter (chondras) of a protoplanetary disk, from the same protoplanetary substance as other planets of the Earth's group of the solar system. Initially, it was small and its structure was more or less homogeneous. But almost immediately inside the proto-Earth, the process of differentiation began - the stratification of the planet's matter with the formation of the core and the shells surrounding it. The first stage of differentiation was the separation of the primary substance into the metal and silicate phases, which led to the formation of a metal core and primitive mantle already in the first 10 million years of the planet's life.

The former residence of the kings of Bora Bora is in the village of Faanui in the northwest, the more or less large settlement of Anau in the east, and most of the expensive hotels are built in the southwest, because there are the best sandy beaches. The island's perimeter is about 30 km. You can rent bikes near the hotel and go exploring the island. Laguna looks gorgeous in all angles. The first European settler on Bora Bora was James Connor, who escaped the wreck of the Matilda whaling ship in 1792. He married a Polynesian and settled on the island's southernmost tip, calling it Matilda Point. Now it's Cape Matira Point, known as one of the island's best beaches.

The magical Bora Bora, like other wonderful islands of Polynesia, was formed after numerous volcanic eruptions that occurred about four million years ago. Today, this most popular island for tourists slowly goes under water. After about twenty-five million years, it will completely sink into the depths of the ocean. Bora Bora is a classic coral atoll, formed on the site of this volcano crater, slowly sinking under the water. The coral belt of the atoll is a visible memory of the former boundaries of the coastline of the volcanic cone. The island's population is about nine thousand people, the locals still honor and do not forget their traditions, which are passed down from generation to generation. He will be happy to show you songs and dances.

The island of Bora Bora is a favorite place for rest and relaxation of world famous celebrities, and for good reason, there is a very relaxing atmosphere. The teeth of the mountains of the main island towering above the shallow turquoise lagoon (the highest ones are Otemanu, Pahia and Mataihua are almost entirely composed of basaltic lava, and the small islands of motu are corals and sand in diameter.

The main attraction of the island of Bora Bora is the lagoon, a place where the richest underwater world prosper. Here live more than half a thousand species of tropical fish, many sharks, barracudas, giant stingrays. You can get acquainted with the wealth of underwater life, dropping into a fascinating underwater journey with a snorkel and a mask, or with an aqualung.

It is known that the Earth is layered: it consists of a core and shells surrounding it - the lower mantle, upper mantle, and the earth's crust. But was she always like that? When, at what stage of earthly history did this stratification take place, and has it completely completed by now? The Earth's mantle is composed of solid rocks, which nevertheless are in a sufficiently plastic state to circulate under the action of heat flows, mixing in a mixer, for billions of years.

It is traditionally believed that the substance composing the bowels of the Earth was so mixed in the process of mantle thermal convection, and even earlier - as a result of deep re-melting and differentiation, that it is no longer possible to detect traces of the primary (protoplanetary) substance from which our planet was formed. However, when studying Pacific island basalts, scientists discovered unusual geochemical anomalies - evidence that reservoirs of primary matter are still preserved in the bowels of the Earth. Researchers studying the Earth tend to look as far as possible into the depths of its history, to understand what and how happened at the earliest stages of the life of our planet. The most obvious way to know the geological past is to study the "stone chronicle" of the oldest rocks.

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