Russia to Evacuate Village for 1st Lunar Lander Mission in Half Century

A jetliner flying from JFK is silhouetted against the moon, Wednesday, Aug. 2, 2023, in New York. (AP Photo/Bebeto Matthews)
A jetliner flying from JFK is silhouetted against the moon, Wednesday, Aug. 2, 2023, in New York. (AP Photo/Bebeto Matthews)
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Russia to Evacuate Village for 1st Lunar Lander Mission in Half Century

A jetliner flying from JFK is silhouetted against the moon, Wednesday, Aug. 2, 2023, in New York. (AP Photo/Bebeto Matthews)
A jetliner flying from JFK is silhouetted against the moon, Wednesday, Aug. 2, 2023, in New York. (AP Photo/Bebeto Matthews)

Russia will evacuate a village in its far east on Aug. 11 as part of the launch of Russia's first lunar lander mission in nearly half a century, a local official said on Monday.

The Luna-25 lunar lander, Russia's first since 1976, will be launched from the Vostochny Cosmodrome, some 3,450 miles (5,550 km) east of Moscow, according to Russia's Roscosmos space agency.

The residents of the Shakhtinskyi settlement in Russia's Khabarovsk region, southeast of the launch site, will be evacuated early morning on Aug. 11, as the village lies in the predicted area where the rocket boosters will fall after they separate.

"The mouth of the Umalta, Ussamakh, Lepikan, Tastakh, Saganar rivers and the area of the ferry crossing on the Bureya River fall into the predicted (booster) fall zone," Alexei Maslov, head of the Verkhnebureinskyi district in the Khabarovsk region, said on the Telegram messaging app. "The residents of Shakhtinskyi will be evacuated."

Luna-25 will launch on a Soyuz-2 Fregat booster and will be the first lander to arrive on the South Pole of the moon, Roscosmos has said.

The main objective of the mission will be the development of soft-landing technologies, research of the internal structure of the Moon and exploration for resources, including water.

The lander is expected to operate on the lunar surface for one year.



Animals Found Living Underground Near Deep-sea Hydrothermal Vents

Giant tubeworms on the seafloor surface at 2,500 meters water depth at the East Pacific Rise, a volcanically active ridge located where two tectonic plates meet on the floor of the Pacific Ocean in this undated photograph.CC BY-NC-SA Schmidt Ocean Institute/Handout via REUTERS
Giant tubeworms on the seafloor surface at 2,500 meters water depth at the East Pacific Rise, a volcanically active ridge located where two tectonic plates meet on the floor of the Pacific Ocean in this undated photograph.CC BY-NC-SA Schmidt Ocean Institute/Handout via REUTERS
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Animals Found Living Underground Near Deep-sea Hydrothermal Vents

Giant tubeworms on the seafloor surface at 2,500 meters water depth at the East Pacific Rise, a volcanically active ridge located where two tectonic plates meet on the floor of the Pacific Ocean in this undated photograph.CC BY-NC-SA Schmidt Ocean Institute/Handout via REUTERS
Giant tubeworms on the seafloor surface at 2,500 meters water depth at the East Pacific Rise, a volcanically active ridge located where two tectonic plates meet on the floor of the Pacific Ocean in this undated photograph.CC BY-NC-SA Schmidt Ocean Institute/Handout via REUTERS

A deep-diving robot that chiseled into the rocky Pacific seabed at a spot where two of the immense plates comprising Earth's outer shell meet has unearthed a previously unknown realm of animal life thriving underground near hydrothermal vents.

Giant tubeworms - the world's heftiest worms - and other marine invertebrates such as snails and bristle worms were found using the remotely operated underwater vehicle SuBastian. They were living inside cavities within the Earth's crust at an ocean-floor site where the Pacific is 1.56 miles (2,515 meters) deep. All the species were previously known to have lived near such vents, but never underground, Reuters reported.

"We discovered vent animal life in the cavities of the ocean's crust. We now know that the unique hydrothermal vent ecosystem extends into the ocean's crust," said marine biologist Sabine Gollner of the Royal Netherlands Institute for Sea Research, one of the leaders of the study published this week in the journal Nature Communications.

"To our knowledge, it is the first time that animal life has been discovered in the ocean crust," Gollner added.

The exploration was conducted at the East Pacific Rise, a volcanically active ridge on the floor of the southeastern Pacific, running approximately parallel to South America's west coast. Earth's rigid outer part is divided into colossal plates that move gradually over time in a process called plate tectonics. The East Pacific Rise is located where two such plates are gradually spreading apart.

This area contains many hydrothermal vents, fissures in the seafloor situated where seawater and magma beneath the Earth's crust come together. Magma refers to molten rock that is underground, while lava refers to molten rock that reaches the surface, including the seafloor. New seafloor forms in places where magma is forced upward toward the surface at a mid-ocean ridge and cools to form volcanic rock.

The hydrothermal vents spew into the cold sea the super-heated and chemical-rich water that nourishes microorganisms.

"The warm venting fluids are rich in energy - for example, sulfide - that can be used by microbes, which form the basis of the food-chain," Gollner said.

Life flourishes around the vents - including giant tubeworms reaching lengths of 10 feet (3 meters), mussels, crabs, shrimp, fish and other organisms beautifully adapted to this extreme environment. The giant tubeworms do not eat as other animals do. Instead, bacteria residing in their body in a sack-like organ turn sulfur from the water into energy for the animal.

The researchers deployed SuBastian from the Schmidt Ocean Institute research vessel Falkortoo to the vent site deep below. The robot was equipped with arms that wielded a chisel that the researchers used to dig into the crust and uncover warm and fluid-filled cavities where the tubeworms, bristle worms and snails were spotted.

"We used a chisel to break the rock. We dug about 20 cm (8 inches). The lava plates were about 10 cm (4 inches) thick. The cavities below the lava plates were about 10 cm in height," Gollner said.

Larvae from these animals may invade these subseafloor habitats, the researchers said, in an example of connectivity between the seafloor and underground ecosystems.

"It changed our view on connectedness in the ocean," Gollner said of discovering the subsurface lair.