Twa kɔ nsɛm atitiriw so
Log in
Sign up for FREE
arrow_back
Laabri

Lesson 4.1 (Geological Timeline)

star
star
star
star
star
Last updated about 2 years ago
15 Nsɛmmisa

This is a map of solar by latitude. Radiation is the

1
1
1
Asemmisa {{asɛmmisaAhyɛnsode}}
1.

Write down 1 notice about the map

Asemmisa {{asɛmmisaAhyɛnsode}}
2.

Write down 1 question you have.

1
Asemmisa {{asɛmmisaAhyɛnsode}}
3.

What do you notice about the annual temperature by latitude?

1
Asemmisa {{asɛmmisaAhyɛnsode}}
4.

The average amount of light in the Arctic is

1
Asemmisa {{asɛmmisaAhyɛnsode}}
5.

Plants use sunlight for photosynthesis. What problems might there be for plants in the Arctic?

Data from scientific studies that used fossils and ice core data indicate that the peat that is part of the peat/permafrost system found today in the Arctic formed approximately 11,000 years ago from living plants that died and have been decomposing ever since at a very slow rate.

It is estimated that there are 1.5 trillion metric tons of organic carbon in the peat/permafrost system. That is a lot of carbon! It is twice as much carbon as what is currently found in the Earth’s atmosphere.

How could enough plants to produce all the carbon found in the peat grow in the Arctic where it is so cold?

1
Asemmisa {{asɛmmisaAhyɛnsode}}
6.

When did the peat that is part of the peat/permafrost system form in the Arctic?

1

Data from the Arctic suggests that 11,000 years ago when the peat formed, the Arctic was a little bit warmer than it is today. There are several factors that could contribute to a warmer Arctic including the tilt of the Earth. Over geologic time, the angle of the Earth’s tilt changes the amount of solar radiation that reaches the surface of the Earth. Currently the tilt of the Earth is 23.5 degrees (nasa.gov). When the plants that formed the peat were growing, the Earth was even more tilted. This means that the Arctic experienced more solar radiation for a longer period of the year. As the tilt of the Earth decreased, less solar radiation was available in the Arctic. The Arctic cooled at this time followed by peat formation and a layer of permafrost.

1
Asemmisa {{asɛmmisaAhyɛnsode}}
8.
1
Asemmisa {{asɛmmisaAhyɛnsode}}
9.

One factor that could have contributed to a warmer Arctic is

1
1
1
1
Asemmisa {{asɛmmisaAhyɛnsode}}
13.

What do you notice about this picture?

1
Asemmisa {{asɛmmisaAhyɛnsode}}
14.
Asemmisa {{asɛmmisaAhyɛnsode}}
15.

Which statement is correct about the peat/permafrost system.

Asemmisa {{asɛmmisaAhyɛnsode}}
7.

How much carbon is estimated to be in the peat/permafrost system?

Asemmisa {{asɛmmisaAhyɛnsode}}
10.

When the plants that formed the peat were growing the Arctic experienced more solar radiation due to the Earth's tilt.

Asemmisa {{asɛmmisaAhyɛnsode}}
11.
Asemmisa {{asɛmmisaAhyɛnsode}}
12.

The Arctic is colder than it was 11,000 years ago because the area gets less sunlight.