What are the four geomorphological depositional landforms?
Drumlins, erratics, moraines, till plains.
What is till?
Unsorted glacial material formed through erosion and weathering.
How do till plains form?
When an ice sheet detaches and melts, depositing till on the valley floor.
Where is till deposited from?
On top of and within the glacier.
How long do till plains last?
A medium-long amount of time.
What can disrupt till plains?
Meltwater, periglacial processes and weathering.
What is an erratic?
A large boulder of a different rock type to surrounding rock.
How are erratics transported?
Broken off by weathering and erosion, transported by a glacier and deposited elsewhere.
When are erratics deposited?
When the glacier loses energy.
How long do erratics last?
Depending on the size, they can last a long time as they are too big to be displaced by weathering alone
What are moraines?
Deposits of eroded material transported with the glacier.
What is a lateral moraine?
Material deposited on the sides of a glacier.
What is a medial moraine?
Formed when two lateral moraines meet in the middle.
What is ground moraine?
Material carried under the glacier and abraded.
What is unique about ground moraine?
It is the only sorted moraine.
What is recessional moraine?
Forms when a retreating glacier stays stationary.
What does recessional moraine show?
Smaller, seasonal retreats.
What is terminal moraine?
Material deposited at the snout of a glacier.
How long do moraines last?
A medium amount of time.
How do drumlins form?
Deposition from underneath glacier builds up behind an obstacle and is dragged over it.
What shape are drumlins?
Tear drop shape.
What are the sides of drumlins called?
Blunt stoss side and tapered lee side.
How large can drumlins be?
Around 1500m long and 100m high.
Where are drumlins found?
In groups called swarms.