Andere Kunden interessierten sich auch für
![Last Glacial Maximum]( "Last Glacial Maximum")
Last Glacial Maximum38,99 €![Return Period]( "Return Period")
Return Period25,99 €![Carbon Cycling in the Glacial Ocean: Constraints on the Ocean¿s Role in Global Change]( "Carbon Cycling in the Glacial Ocean: Constraints on the Ocean¿s Role in Global Change")
Carbon Cycling in the Glacial Ocean: Constraints on the Ocean¿s Role in Global Change74,99 €![Late Quaternary Sea-Level Correlation and Applications]( "Late Quaternary Sea-Level Correlation and Applications")
Late Quaternary Sea-Level Correlation and Applications39,99 €![Glacial Isostasy, Sea-Level and Mantle Rheology]( "Glacial Isostasy, Sea-Level and Mantle Rheology")
Glacial Isostasy, Sea-Level and Mantle Rheology229,99 €![Field Techniques in Glaciology and Glacial Geomorphology]( "Field Techniques in Glaciology and Glacial Geomorphology")
Field Techniques in Glaciology and Glacial Geomorphology76,99 €![Past Glacial Environments]( "Past Glacial Environments")
Past Glacial Environments89,99 €
Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. A glacial period is an interval of time within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate within an ice age. The last glacial period ended about 10,000 to 15,000 years ago; the current Holocene epoch is the interglacial we are presently in.