BITS ‘N’ PIECES
Narrated Ibn Mas`ud
The Prophet (S.A.W) used to take care of us in preaching by selecting a suitable time, so that we might not get bored. (He abstained from pestering us with sermons and knowledge all the time).
Sahih Bukhari, Volume 1, Book 3, Number 68
In a dramatic collision of nature’s forces, a colossal iceberg, nearly half the size of Rhode Island, recently crashed into a penguin sanctuary in Antarctica. Named D-30A, this massive tabular iceberg, stretching 45 miles in length and 12.5 miles in width, originated from a similar collision two years prior. Despite its imposing size, the impact seems to have caused minimal damage, leading to an intriguing series of events.
D-30A’s story begins in June 2021 when its parent iceberg, D-28, collided with the land near the Borchgrevink Ice Shelf in eastern Antarctica, splitting into two. Since then, D-30A has slowly drifted westward along the Antarctic coast, largely unnoticed. However, in late 2022, it took an unexpected turn, setting its course for Clarence Island, the easternmost of the South Shetland Islands.
Clarence Island is a crucial breeding ground for chinstrap penguins, hosting around 100,000 breeding pairs each winter. Concerns arose that the iceberg’s collision could devastate this vulnerable population. Fortunately, timing was on their side, as the penguins had not yet returned to the colony. Had the collision occurred a few months later, it could have had severe consequences.
Icebergs colliding with islands can wreak havoc on wildlife, disrupting marine animal migration and affecting the temperature and salinity of surrounding waters. The scraping of icebergs across the seafloor can harm seafloor ecosystems and disrupt the local food web.
Clarence Island’s deep seafloor likely prevented D-30A from becoming stranded. Its eastern side features a steep drop-off with deep water, allowing the iceberg to pass through without obstruction. Even so, if the penguins had been nesting on the island, a blocked access to the colony for just a few days could have led to a breeding catastrophe.
Surprisingly, the close encounter with D-30A may have a silver lining for the local wildlife. As the iceberg passed by, it released iron-rich meltwater, potentially promoting increased algal growth in the area, benefiting the ecosystem.
Currently, D-30A is on a course into the Drake Passage, known as “iceberg alley,” where ocean currents can drag massive icebergs into warmer waters, leading to their eventual demise. This recent event serves as a reminder of the unpredictable nature of Antarctic ice, where even colossal icebergs play a delicate role in the balance of the ecosystem.