PTE · Listening: Fill in the Blanks

Dynamics and Life of Icebergs: PTE Listening: Fill in the Blanks practice questions

3 original Listening: Fill in the Blanks questions. Answer every question, then check them for your score and the answers. It is free with no login; create a free account to save your score and get a BandLadder AI score for speaking and writing.
  • 3 questions
  • Free, with answers
  • PTE Academic and PTE Core
  • Updated Oct 2026

You will hear a recording. Type the missing word in each gap.

1

Nutrient Dispersal from Melting Ice

Speaker: British English

Plays once, as in the test: no pausing or replay

0:00 / 0:51

As massive tabular icebergs drift into warmer ocean currents, they release vast quantities of trapped mineral dust into the surrounding seawater. This process of melting introduces essential iron particles that stimulate the rapid growth of marine communities. Scientists monitoring these drift zones have observed substantial increases in biological across several hundred square kilometres. The resulting organic material not only supports regional food webs but also aids the long term of atmospheric carbon as dead matter sinks to the seafloor. Consequently, these drifting frozen giants act as mobile fertiliser factories that enrich otherwise barren oceanic over several months.

2

Acoustic Monitoring of Calving Events

Speaker: American English

Plays once, as in the test: no pausing or replay

0:00 / 0:41

Marine scientists increasingly rely on underwater acoustic instruments to record the soundscapes generated by polar ice shelves. When a major fracture develops within a glacier, it produces powerful low frequency rumblings that across vast oceanic distances. These hydroacoustic signals allow researchers to detect sudden structural long before satellite images can confirm the separation of a new iceberg. Detailed analysis of these underwater recordings provides valuable insights into how thermal stress and ocean waves ice disintegration. By measuring the intensity of these acoustic pulses, geophysicists can estimate the volume of ice detached during each major calving event.

3

Deterioration Mechanisms of Ice Masses

Speaker: Australian English

Plays once, as in the test: no pausing or replay

0:00 / 0:49

Once an iceberg becomes detached from an ice shelf, its physical structure undergoes rapid deterioration driven by multiple environmental factors. Surface warmth generates meltwater that pools on top and widens existing through hydraulic pressure. At the same time, turbulent sub surface currents erode the submerged base, creating an unstable that causes the entire mass to capsize. This dramatic rolling action exposes fresh surfaces to sunlight and accelerates the of the remaining core into smaller fragments. Such rapid decay presents a major hazard for maritime navigation, as smaller floating pieces are far more to detect on radar systems.

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