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The Iberian orca subpopulation lives in the coastal waters of the Iberian Peninsula and is genetically distinct from other orca populations in the Northeast Atlantic. [1] The orcas follow the seasonal migration of Atlantic bluefin tuna (Thunnus thynnus), their primary food source, gathering in the early spring in the Strait of Gibraltar ...
Why Iberian orcas are attacking ships in the Strait of Gibraltar, one of the world’s busiest waterways, has quickly become one of the terrifying mysteries of the sea.
The killer whales regularly demonstrate their competence by chasing seals up shelving gravel beaches, up to the edge of the water. The pursuing whales are occasionally partially thrust out of the sea by a combination of their own impetus and retreating water, and have to wait for the next wave to re-float them and carry them back to sea. [12]
With large waves, this crash can be felt by beachgoers on land. Offshore wind conditions can make plungers more likely. If a plunging wave is not parallel to the beach (or the ocean floor), the section of the wave which reaches shallow water will break first, and the breaking section (or curl) will move laterally across the face of the wave as ...
More than 250 boats have been damaged by orcas since 2020, with 15 of Iberia’s orcas believed to be responsible Orca boat rammings in the Mediterranean are ‘just playful fad’ scientists say ...
The orca repeatedly lunged out of the water, attempting to reach her trainer. The incident was caught on video by an audience member. Critics of marine parks have blamed lack of companionship for Shouka's aggression, as she did at one time have a companion bottlenose dolphin named Merlin who was subsequently moved to another area of the park.
A pod of killer whales bumped one of the boats in an endurance sailing race as it approached the Strait of Gibraltar, the latest encounter in what researchers say is a growing trend of sometimes ...
The "neck" is where the flow is most rapid. When the water in the rip current reaches outside of the lines of breaking waves, the flow disperses sideways, loses power, and dissipates in what is known as the "head" of the rip. Rip currents can form by the coasts of oceans, seas, and large lakes, whenever there are waves of sufficient energy.