interglacial
C2Technical/Scientific
Definition
Meaning
A geological period of warmer climate between two glacial periods (ice ages).
A period of relative warmth and climatic stability occurring between extended cold phases in Earth's history, characterized by retreat of ice sheets and changes in flora and fauna.
Linguistics
Semantic Notes
Used almost exclusively in geology, climatology, and paleontology. In these fields, it refers to formally defined geological periods (e.g., Eemian interglacial). The term implies a cyclical, recurring pattern within the larger framework of ice age cycles.
Dialectal Variation
British vs American Usage
Differences
No significant differences in meaning or usage. Both dialects use the term identically within scientific contexts. Spelling is identical.
Connotations
Neutral scientific term in both dialects. Carries connotations of natural climate cycles and Earth history.
Frequency
Extremely rare in general discourse in both regions. Frequency is identical and confined to academic/scientific publications.
Vocabulary
Collocations
Grammar
Valency Patterns
[the] + interglacial + (period/stage)[adjective: last/previous/present] + interglacialduring + the + interglacialVocabulary
Synonyms
Strong
Neutral
Weak
Vocabulary
Antonyms
Phrases
Idioms & Phrases
- “[No established idioms for this technical term]”
Usage
Context Usage
Business
Virtually never used.
Academic
Primary domain of use. Essential in geology, earth sciences, climatology, archaeology, and paleontology to describe specific phases of Quaternary climate history.
Everyday
Extremely rare, only in discussions of climate change history or popular science media.
Technical
Precisely defined term with specific chronological and climatic parameters (e.g., specific temperature thresholds, sea-level markers).
Examples
By Part of Speech
verb
British English
- [No standard verb form]
American English
- [No standard verb form]
adverb
British English
- [No standard adverb form]
American English
- [No standard adverb form]
adjective
British English
- The research focused on interglacial sediments in the North Sea basin.
- Interglacial conditions allowed forests to expand northwards.
American English
- Scientists studied interglacial coral reefs in the Florida Keys.
- The model simulates interglacial temperature patterns.
Examples
By CEFR Level
- [Too complex for A2. Use simpler phrase: 'a warm time between ice ages.']
- The last interglacial period was warmer than today.
- Ice ages are followed by interglacial periods.
- Sea levels were several metres higher during the last interglacial.
- The current Holocene epoch is an interglacial period.
- Palaeoclimatologists use deep-sea cores to date past interglacials.
- The duration and stability of the present interglacial is a key concern for future climate projections.
Learning
Memory Aids
Mnemonic
Think: INTERnational GLACIAL break. Between (INTER) two icy (GLACIAL) ages is a break or warmer period.
Conceptual Metaphor
EARTH'S CLIMATE IS A PENDULUM SWINGING BETWEEN ICE AND WARMTH.
Watch out
Common Pitfalls
Translation Traps (for Russian speakers)
- Avoid direct calque 'межледниковый' unless in exact scientific context. In general description, 'теплый период между ледниковыми периодами' is clearer.
- Do not confuse with 'interstellar' (межзвездный).
Common Mistakes
- Using it as an adjective for any warm break in cold weather (e.g., 'We had an interglacial week in January' – incorrect).
- Confusing 'interglacial' (long, formal period) with 'interstadial' (shorter warm phase within a glacial period).
Practice
Quiz
What is an 'interglacial'?
FAQ
Frequently Asked Questions
Yes, the current geological epoch, the Holocene, which began about 11,700 years ago, is considered an interglacial period within the ongoing Quaternary ice age.
Past interglacials have varied in length, but typically last between 10,000 to 30,000 years. The current Holocene interglacial is already about 11,700 years old.
An interglacial is a full, long-duration warm period between major glacial periods (ice ages). An interstadial is a shorter, milder warm phase that occurs within a larger glacial period, not ending it.
Human-induced climate change is radically altering the natural trajectory of the current interglacial. Instead of a gradual cooling towards the next glacial, we are causing rapid warming, potentially shortening or drastically modifying the natural interglacial cycle.