User:Auricolour/sandbox

To-Do List

 * work on Stadial
 * work on Ichnofacies
 * Table of Marine Isotope Stages
 * Authigenesis
 * Fortunian
 * Fossil Hash
 * Earth Pigment
 * Lithification
 * Bleb (mineralogy)
 * stop browsing through stubs

German
For the most part, there is a very misunderstanding of the terms Ice Age / Ice Age, Warm Time / Interglacial, Cold Time / Glacial, Stadial and Interstadial. All these pairs of terms have different meanings and are not synonyms for each other.

Each glacial and interglacial was (with naturally fundamentally cold or warm climate) characterized by smaller temperature fluctuations with slightly warmer and again slightly colder periods, which extended over several centuries to millennia. However, these relatively short-lived climatic variations (compared to the duration of the total glacier considered) did not affect the relationship between snow accumulation and ablation of the inland ice and glaciers.

Spanish
https://es.wikipedia.org/wiki/Estadial the entire article is gold

Dutch
The growth and retreat of glaciers can best be reconstructed for the last glacial (the Weichsel or Würgglacial), because the traces in the geomorphology left by the glaciers are still "fresh". During this glacial several stadials and interstadials can be recognized, the latter being:

the Older Dryas city from 12,900 to 12,700 years ago the Allerød interstadial from 12,700 to 11,900 years ago the Younger Dryas city from 11,900 to 10,700 years ago The Younger Dryas is the last period in which the glaciers gained ground, the period thereafter is defined as the Holocene.

Norwegian
The stadiums from the last ice age (Weichsel) are best known. Stadialer from this ice age is the Herning Stadium for 115,000-105,000 years ago (isotope stage 5d), the Rederstall stadium for 93,000-85,000 years ago (isotope stage 5b) and the Schalkholz stadium for 71,000-57,000 years ago (isotope stage 4).