Glacial landscapes Flashcards
and climate reconstruction
What two national parks in the UK can show us evidence that the UK used to be glacialated?
The Lake District and Snowdonia
What is Palynology and how it is useful?
- It is the study of pollen fossils
- Used to analyse past environments, climate and ecosystem
What is a Diatom?
- They are aqautic microscopic unicellular algae
- Absorb nutrients and CO2 from water
- Used to reconstruct past environements
Moraine
- Medial, formed from two lateral morainesnmeeting in the middle of a glacier
- Lateral, material deposited on the glacier side, leaving an ridge when the glacier melts
- Reccessional, formes at the end of a glacier when a retreating glacier stays stationary for a long period of time
- Terminal, material deposited at the snout of the glacier on valley floor
Drumlins
Elongated hills of glacier deposition, made of material accumulation under glacier
Till plains
(Lowland), Till becoming deposited when icesheet detach from glacier body
Ablation till
(Lowland), accumulation of till by the melting of stagant ice
Aretes
A knife edged ridge formed from erosion of two corrie backwalls
Pyramid peaks
formed from erosion between three or more corries, producing a peak
Glacial troughs
Erosion grinds a v-shaped valley into a U
Truncated spurs
Formed when a glacier cuts and erodes interlocking spurs
Hanging valley
Main valley erodes eroses quicker than tributary valley
Ribbon lake
An area of soft rock is eroded more readily than surrounding hard rock on valley floor. Plucking and abrasion create hollows that fill up with rain water
Rouche mountonnees
Small rocks are not always removed and becomes polished by abrasion
Knock and Lochan
A scoured lowlad which displays alternating Rouch moutonnees and small lakes