How Far Is 3000 Metres – Athletes run 3,000 meters, but the exact number of laps depends on the location of the jump and whether the track is inside or outside the second turn. Athletes begin to group together and can immediately break inside.
Competitors must consecutively clear 28 fixed obstacles and seven water jumps for the duration of the race. The order of completion is determined in time.
How Far Is 3000 Metres
The height of the male threshold is 36 inches (91.4 cm) and the female threshold is 30 inches (76.2 cm). The water jump landing area was 12 feet (3.66 m) long and 70 cm deep.
Men’s 3000 Meters Steeplechase Results; El Bakkali Cruising
This event is of British origin; Runners will run from one city face to another and jump over obstacles like streams and low walls. The current event can be traced back to the mid-19th century Oxford University two-mile steeplechase, which was established as a track event, with steeplechase, at the British Year Championships. 1879
Current format At every Olympics since 1900, men have competed – initially at different distances.
Perhaps no country dominates an event quite like Kenya does in tower crossing. Since Amos Biwott won the gold medal at the 1968 Olympics, Kenya has won all but two men’s Olympic tower titles until 2016. In women’s hurdles, Russia, Tunisia and Bahrain won the 2008, 2012 and 2016 Olympic championships, respectively. – August 1, 2021. Hiwin Kieng of Kenya and Mekides Abebe of Ethiopia in action / Alexandra Schmigiel
TOKYO, Aug 1 () — Under a scorching Tokyo sun, the women’s 3,000m steeplechase began their quest for Olympic immortality on Sunday as favorites Hiwin Kieng Kenya reached the final amid extreme temperatures at the Olympic Stadium on Wednesday. .
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Kieng, the 2015 world champion and silver medalist in Rio five years ago, will be hoping for gold this time around as he wins his heat with a controlled, timed run of 9:23.17 as temperatures hit 30 degrees on the track.
She will be joined in the final by compatriot Beatrice Cepkoec, the 2019 world champion who broke the 2018 world record in Monaco with a stunning 8:44.32.
At the Olympic Stadium on Sunday, Chepkoech took his time in his race, apparently to conserve energy, and finished third in 9:19.82, good enough to earn a spot in the medal round.
“I feel good, although I have a little problem,” he said without elaborating.
The Ocean Zones
But it won’t be easy for the Kenyans and among those aiming for a podium finish is Asian Games gold medalist Winfred Mutile Yawi of Bahrain, who won his race in 9:10.80, the fastest of the matches. .
Also competing will be American Courtney Frieich, who impressively beat Chepkoech to win her race in 9:19.34.
“It’s all about qualifying. But my separation (clearly at the front) pretty easily gave me confidence and I felt comfortable,” he said after the race.
The 2017 world silver medalist will join compatriot Emma Coburn in the medal hunt after she clocked 9:16.91 to finish third, good enough to send her into the final.
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African Games champion Mekides Abebe of Ethiopia, 20, who clocked the year’s second-fastest finish of 9:02.52, advanced to the final after finishing third in his heat. The ocean is divided into different regions based on depth relative to the surface to be understood by oceanographic studies.
The ocean covers more than 70% of the Earth’s total surface area and contains about 97% of its total water. With an area of about 361.9 million square kilometers, it is a vast continuous body of salt water, so large that oceanographers estimate that less than 20% has been discovered. Although there is one global ocean, it is generally divided into five major basins: the Pacific, Atlantic, Indian, Southern, and Arctic oceans.
With an average depth of 3,700 meters, experts have also divided the world’s oceans into different regions based on surface depth to facilitate oceanographic research. The ocean is divided into zones based on the distance light can reach:
This sunlit region, also known as the superficial or epithelial zone, named after its location at the surface, extends to less than 200 meters or about 5% of the average ocean depth. In the afternoon, it is almost completely illuminated by the sun, hence the so-called sunlight zone. It is also considered the warmest layer. More natural light also generates heat that penetrates deeper into the water due to wind movement. Depending on the location, the temperature of the epithelium can rise as high as 97 degrees F or fall as low as 28 degrees. Enough sunlight penetrates this layer for algae to use for photosynthesis, which in turn produces about 50% of the oxygen in our atmosphere. The shallow zone is home to most commercial fisheries and is home to a wide variety of animals, including whales, dolphins and sharks, many of which regularly breach the ocean’s surface.
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The twilight zone or mesosphere begins at a depth of 200 meters and extends to 1000 meters, which is about 20% of the total depth of the ocean. It is usually a very dark place, but in the afternoon it receives a little sunlight, which is enough for photosynthesis. The twilight zone actually plays a major role in regulating our planet; The oceans absorb about 25% of the carbon dioxide that humans emit and push it into the deep ocean, preventing it from returning to the atmosphere. Unlike the surface zone, this second layer remains relatively untouched by commercial fishing, even though it teems with aquatic life. The mesopelagic region is also where experts first observed the presence of bioluminescent organisms. The temperature variation here is the most extreme. This is partly due to heat flux, a transition zone where warm water falls rapidly.
The deep ocean—the third and final layer—extends from the 1,000-meter point to the ocean floor, whatever that depth is. At least it covers 75% of the ocean’s depth. It was a cold area that received absolutely no natural light. The organisms living in this area are bioluminescent; That is, they create and emit their own light. Examples of these creatures include certain species of plankton, jellyfish, squid, and nightmarish spiny worms. They live in complete darkness, have light-sensitive eyes that allow them to sense each other’s presence. The deep ocean is divided into 3 zones: the midnight zone, the abyss and the trench
The midnight zone, also known as the swimming zone, occupies the first third of the deep ocean according to the three-layer model. It extends from 1000 meters to 4000 meters – about the average depth of the global ocean. The temperature rarely changes and remains fairly constant at 39 degrees Fahrenheit. As mentioned earlier, the only light in these regions does not come from the sun, but from bioluminescent animals that use bioluminescence. They use their skills to hunt or find mates. Some spend their days in complete darkness. However, there are some sea creatures that swim this far for food, such as sperm whales. In fact, at 15 times the size of the epithelium, the underwater sea is often considered the world’s largest ecosystem.
The abyssopelagic zone is the middle layer of the deep ocean. Its name comes from Greek
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Means “without a root”. As the name suggests, there was a time when the ancients believed that the ocean was a bottomless void. It extends from 4,000 meters to 6,000 meters for some global zones that mark the bottom of the sea. The water temperature never exceeds freezing. There is a surprising lack of life in the Abyss; Only a few organisms can survive high pressure, such as invertebrates.
The trench (hadalpelagic zone) is the deepest part of the ocean. It extends across the gap wherever possible in the world; This usually occurs in the form of deep sea trenches and canyons. An example of such a miracle is the Mariana Trench in the Pacific Ocean, which marks the deepest point on Earth at 11,034 meters, a depth so deep that Mount Everest would sink completely if it were to go under. The pressure is so strong that it is equivalent to the approximate weight of 48 Boeing 747 airplanes. Nevertheless, life exists in this area. The
An ocean is a large body of water that covers more of the Earth’s surface than land. Despite this, professional oceanographers tried to divide it into different classes. Although there is overlap between the three and five layer concepts, especially in the first two
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