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Here are additional clues for each of the words in today's Mini Crossword. NYT Mini Across Hints 1 Across: Square on a wall calendar, or a fun thing you might put on the calendar — HINT: It ...
From c. 200 to c. 290 there was a period of cooling, which affected the northwestern provinces of the Empire. [3] Dendrochronology indicates that severe drought which began in 338 and persisted until 377 forced the nomadic pastoral federation of Huns to seek pastures and predation farther to the west and south. [ 3 ]
A plural clue always indicates a plural answer and a clue in the past tense always has an answer in the past tense. A clue containing a comparative or superlative always has an answer in the same degree (e.g., [Most difficult] for TOUGHEST). [6] The answer word(s) will not appear in the clue itself. The number of words in the answer is not ...
The Younger Dryas (YD, Greenland Stadial GS-1) [2] was a period in Earth's geologic history that occurred circa 12,900 to 11,700 years Before Present (BP). [3] It is primarily known for the sudden or "abrupt" cooling in the Northern Hemisphere, when the North Atlantic Ocean cooled and annual air temperatures decreased by ~3 °C (5 °F) over North America, 2–6 °C (4–11 °F) in Europe and ...
Play the USA TODAY Crossword Puzzle.. Sunday Los Angeles Times crossword Sunday New York Times crossword Sunday Premier crossword SUDOKU. Play the USA TODAY Sudoku Game.. JUMBLE. Answer: PUDDLE ...
The Late Antique Little Ice Age is seen between the middle of the 6th century and the start of the 7th century, and preceded by the Roman Warm Period. [1]The Late Antique Little Ice Age (LALIA) was a long-lasting Northern Hemispheric cooling period in the 6th and 7th centuries AD, during the period known as Late Antiquity.
The Older Dryas is a period of cooling during the Bølling–Allerød warming, estimated to be from 13,900 to 13,600 years before present (BP), [7] and the estimated ages can vary using different age dating methods. Numerous studies on chronology and palaeoclimate of last deglaciation show a cooling event within Bølling–Allerød warming that ...
This decline in population meant that cultivated lands became unkempt, allowing for the regrowth of wild plants. This is thought to have caused the drop in atmospheric carbon dioxide in the sixteenth century that exacerbated the extreme cooling period. However, depopulation is the least significant of the causes of the Grindelwald Fluctuation. [15]