Total Pageviews

Saturday, February 29, 2020

Ice Age- A geological period of temperature reduction

An ice age is 
a long period
when Earth's 
surface and 
atmosphere 
are much colder
than average.

That results in 
continental and 
polar ice sheets, 
and alpine glaciers. 

Earth's 
climate 
alternates 
between 
ice ages and 
greenhouse 
periods.

During greenhouse 
periods, there are 
no glaciers at all. 

Earth is currently 
in the Quaternary 
glaciation.
( aka "Ice Age" )

Within an ice age 
are very cold 
"glacial periods" 
and warm periods, 
called "interglacials".

"Ice age" 
implies 
extensive
ice sheets 
in both the 
northern and 
southern 
hemispheres.

We are living 
in a "warm" 
interglacial 
period called
the Holocene. 



Three types 
of evidence 
for ice ages: 

Geological Evidence:
Rock scouring 
and scratching, 
glacial moraines, 
drumlins, valley 
cutting, the 
deposition of 
till or tillites and 
glacial erratics. 

Sediment and 
ice cores studies
reveal that glacials 
last a long time, 
but interglacials 
are short periods. 



Chemical Evidence:
Variations in the 
ratios of isotopes 
in fossils present 
in sediments,
sedimentary rocks 
and ocean sediment 
cores. 



Paleontological Evidence:
Changes in the 
geographical 
distribution 
of fossils. 

During a cold
glacial period 
living creatures 
will move to lower, 
warmer latitudes, 
or become extinct.



There have been 
at least five major 
ice ages:

(1) Huronian, 
2.4 to 2.1 billion years ago, 
during the early 
Proterozoic Eon. 

(2) Cryogenian, 
720 to 630 million years ago, 

(3) Andean-Saharan, 
460 to 420 million years ago.

(4) late Paleozoic,
360 to 260 million years ago. 

 (5) Quaternary,
Started about 2.58 million 
years ago.

2.58 million years ago 
is based on formation 
of the Arctic ice cap.

The Antarctic ice sheet 
began to form about 
34 million years ago.

There have been 
cycles of glaciation, 
with ice sheets 
advancing 
and retreating, 
on 40,000-year 
and 100,000-year 
time scales.

The Earth 
is now 
in a warm
interglacial 
warm period.

The last cold 
glacial period 
ended about 
10,000 years 
ago. 

All that remains
of the continental 
ice sheets are
the Greenland 
and Antarctic 
ice sheets, and 
some smaller 
glaciers.


Outside of ice ages, 
the Earth seems 
to have been ice free, 
even in high latitudes, 
in periods known as 
greenhouse periods.