Moraine Internal Structure and Form

Toby Tonkin; Nicholas Midgley

Moraine Internal Structure and Form

Toby Tonkin
, Nicholas Midgley

Research output: Contribution to Book/Report › Chapter

Abstract

Moraines are ridges or mounds of unconsolidated sediment (loose, deposited materials) that develop at the margins of glaciers. Whilst the glaciers of the Tarfala valley in northern Sweden are well studied in terms of their glaciology, the moraines are less well understood. The sedimentary composition, internal structure and morphology (shape) of moraines is related to a range of glaciological and surface processes. Therefore these landforms can be seen as an archive of past glacier characteristics and activity. Studies of these landforms may contribute to our understanding of the character and behaviour of these glaciers over a range of timescales and therefore merit further investigation.

Original language	English
Title of host publication	INTERACT - Stories of Arctic Science
Editors	Terry V. Callaghan, Hannele Savela
Place of Publication	Aarhus
Publisher	Aarhus University
Chapter	1.4
Pages	40-41
Number of pages	2
ISBN (Print)	978-87-93129-11-5
Publication status	Published - 2015
Externally published	Yes

Bibliographical note

This book contains stories of cutting-edge Arctic research supported by INTERACT Transnational Access. INTERACT Stories of Arctic Science has been edited by INTERACT Coordinator Terry V. Callaghan and Transnational Access Coordinator Hannele Savela. The preface has been written by Her Royal Highness Crown Princess Victoria of Sweden.

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Tonkin_Midgley_INTERACT_2015_Moraine_internal_structure_and_formFinal published version, 1.06 MBLicence: CC BY

http://10.2312/GFZ.LIS.2015.002Licence: CC BY

Cite this

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title = "Moraine Internal Structure and Form",

abstract = "Moraines are ridges or mounds of unconsolidated sediment (loose, deposited materials) that develop at the margins of glaciers. Whilst the glaciers of the Tarfala valley in northern Sweden are well studied in terms of their glaciology, the moraines are less well understood. The sedimentary composition, internal structure and morphology (shape) of moraines is related to a range of glaciological and surface processes. Therefore these landforms can be seen as an archive of past glacier characteristics and activity. Studies of these landforms may contribute to our understanding of the character and behaviour of these glaciers over a range of timescales and therefore merit further investigation. ",

author = "Toby Tonkin and Nicholas Midgley",

note = "This book contains stories of cutting-edge Arctic research supported by INTERACT Transnational Access. INTERACT Stories of Arctic Science has been edited by INTERACT Coordinator Terry V. Callaghan and Transnational Access Coordinator Hannele Savela. The preface has been written by Her Royal Highness Crown Princess Victoria of Sweden.",

year = "2015",

language = "English",

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TY - CHAP

T1 - Moraine Internal Structure and Form

AU - Tonkin, Toby

AU - Midgley, Nicholas

N1 - This book contains stories of cutting-edge Arctic research supported by INTERACT Transnational Access. INTERACT Stories of Arctic Science has been edited by INTERACT Coordinator Terry V. Callaghan and Transnational Access Coordinator Hannele Savela. The preface has been written by Her Royal Highness Crown Princess Victoria of Sweden.

PY - 2015

Y1 - 2015

N2 - Moraines are ridges or mounds of unconsolidated sediment (loose, deposited materials) that develop at the margins of glaciers. Whilst the glaciers of the Tarfala valley in northern Sweden are well studied in terms of their glaciology, the moraines are less well understood. The sedimentary composition, internal structure and morphology (shape) of moraines is related to a range of glaciological and surface processes. Therefore these landforms can be seen as an archive of past glacier characteristics and activity. Studies of these landforms may contribute to our understanding of the character and behaviour of these glaciers over a range of timescales and therefore merit further investigation.

AB - Moraines are ridges or mounds of unconsolidated sediment (loose, deposited materials) that develop at the margins of glaciers. Whilst the glaciers of the Tarfala valley in northern Sweden are well studied in terms of their glaciology, the moraines are less well understood. The sedimentary composition, internal structure and morphology (shape) of moraines is related to a range of glaciological and surface processes. Therefore these landforms can be seen as an archive of past glacier characteristics and activity. Studies of these landforms may contribute to our understanding of the character and behaviour of these glaciers over a range of timescales and therefore merit further investigation.

M3 - Chapter

SN - 978-87-93129-11-5

SP - 40

EP - 41

BT - INTERACT - Stories of Arctic Science

A2 - Callaghan, Terry V.

A2 - Savela, Hannele

PB - Aarhus University

CY - Aarhus

ER -

Moraine Internal Structure and Form

Abstract

Bibliographical note

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