Episode 1: Reaching the mid-Miocene ΡΠΊΠ°ΡΠ°ΡΡ Π² Ρ ΠΎΡΠΎΡΠ΅ΠΌ ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅
Episode 1: Reaching the mid-Miocene
7 years ago
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Π£ Π½Π°Ρ Π²Ρ ΠΌΠΎΠΆΠ΅ΡΠ΅ ΠΏΠΎΡΠΌΠΎΡΡΠ΅ΡΡ Π±Π΅ΡΠΏΠ»Π°ΡΠ½ΠΎ Episode 1: Reaching the mid-Miocene ΠΈΠ»ΠΈ ΡΠΊΠ°ΡΠ°ΡΡ Π² ΠΌΠ°ΠΊΡΠΈΠΌΠ°Π»ΡΠ½ΠΎΠΌ Π΄ΠΎΡΡΡΠΏΠ½ΠΎΠΌ ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅, Π²ΠΈΠ΄Π΅ΠΎ ΠΊΠΎΡΠΎΡΠΎΠ΅ Π±ΡΠ»ΠΎ Π·Π°Π³ΡΡΠΆΠ΅Π½ΠΎ Π½Π° ΡΡΡΠ±. ΠΠ»Ρ Π·Π°Π³ΡΡΠ·ΠΊΠΈ Π²ΡΠ±Π΅ΡΠΈΡΠ΅ Π²Π°ΡΠΈΠ°Π½Ρ ΠΈΠ· ΡΠΎΡΠΌΡ Π½ΠΈΠΆΠ΅:
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Episode 1: Reaching the mid-Miocene
Episode 1: Reaching the mid-Miocene The scientists of Expedition 374: Ross Sea West Antarctic Ice Sheet History have completed coring at their first site. They brought up cores that revealed the presence of former glaciations and reached back in time about 16 million years to the period of geologic history known as the mid-Miocene. The mid-Miocene is important because it is the last period in Earth's history when Earth was as at it's warmest, similar to how it is today. Because of this past warmth, the mid-Miocene may provide an analog to what lies in store in a future warmer climate. Watch coring begin and the scientists explain in this video.
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