TOPIC:
GEOMORPHOLOGY:MEANING, &
SCOPE….
APOORVA MATHUR
The rapidly evolving discipline of
geomorphology has undergone
seachange in methodology and
approaches to landforms and related
processes.
INTRODUCTION
MEANING:-
Geomorphology is significant branch of physical
geography(geomorphology,oceanography,clim
atology and biogeography).
The geomorphology stems
from three GREEK WORDS i.e. ‘ge’(meaning
earth), ‘morphe’(form) and ‘logos’(a
discourse).
DEFINITION
It is defined as the science of description of
various forms of the earth’s surface.
Geomorphology may be defined
as the systematic description and analysis of
landscapes and the processes that change
them.
-A.L.Bloom
SCOPE OF GEOMORPHOLOGY
The subject matter of
geomorphology may be
organised on the basis of
1.Dimension and scale of
relief features(landforms);
2.Processes that shape the
landforms and
3.The approaches to the
geomorphic studies.
Process geomorphology has evolved into
subfields of specializtion such as
hillscope morphology,fluvial
processes,karst,volcanic,arid,eolian,
glacial and coastal geomorphology-to
name only some of the better known.
To illustrate the concept of geomorphic
description in terms of structure,process,and
tme,consider the following two descriptive
paragraphs.
The first is empirical;it states what
and where;
The second is explanatory;it denotes how as
well as what and where.
On the basis of
dimension and
scale,the relief
features of the earth’s
surface the core
subject matter of
geomorphic
study,may be grouped
in 3 broad categories
of descending order.
1.RELIEF FEATURES OF
THE FIRST ORDER
2.RELIEF FEATURES OF
THE SECOND ORDER
3.RELIEF FEATURES OF
THE THIRD ORDER
Respectively.
RELIEF FEATURES OF THE FIRST ORDER
On the smallst scale and covering the largest area is
the ‘world geomorphology’.
which includes consideration of continents
and ocean basins consideration and
interpretation of worldwide erosion surfaces
requires the analysis of the characteristics and
evolution of continents and ocean basins.
Eg:plate tectonics help in understanding
the origin of continents and ocean basins.
RELIEF FEATURES OF THE SECOND
ORDER
The structural forms developed over a continent
part thereof as
mountains,plateaus,lakes,faults,rift valleys
etc.
constitute the category of relief
features of the second order.
These are also known as “constructional
landforms”.
RELIEF FEATURES OF THE THIRD
ORDER
Micro –level landforms developed on second
order relief features by exogenic denudational
processes originating from the atmosphere
are included in this category.
these landforms may be
erosional(glacial valleys,river valley,karst valley
etc) and depositional (drumlins,flood
plains,inselbergs etc) and sometimes minor
tectonics features(by endogenetic forces).
THANKYOU

Geomorpholgy: NATURE AND SCOPE

  • 1.
  • 2.
    The rapidly evolvingdiscipline of geomorphology has undergone seachange in methodology and approaches to landforms and related processes. INTRODUCTION
  • 3.
    MEANING:- Geomorphology is significantbranch of physical geography(geomorphology,oceanography,clim atology and biogeography). The geomorphology stems from three GREEK WORDS i.e. ‘ge’(meaning earth), ‘morphe’(form) and ‘logos’(a discourse).
  • 4.
    DEFINITION It is definedas the science of description of various forms of the earth’s surface. Geomorphology may be defined as the systematic description and analysis of landscapes and the processes that change them. -A.L.Bloom
  • 5.
    SCOPE OF GEOMORPHOLOGY Thesubject matter of geomorphology may be organised on the basis of 1.Dimension and scale of relief features(landforms); 2.Processes that shape the landforms and 3.The approaches to the geomorphic studies.
  • 6.
    Process geomorphology hasevolved into subfields of specializtion such as hillscope morphology,fluvial processes,karst,volcanic,arid,eolian, glacial and coastal geomorphology-to name only some of the better known.
  • 7.
    To illustrate theconcept of geomorphic description in terms of structure,process,and tme,consider the following two descriptive paragraphs. The first is empirical;it states what and where; The second is explanatory;it denotes how as well as what and where.
  • 8.
    On the basisof dimension and scale,the relief features of the earth’s surface the core subject matter of geomorphic study,may be grouped in 3 broad categories of descending order. 1.RELIEF FEATURES OF THE FIRST ORDER 2.RELIEF FEATURES OF THE SECOND ORDER 3.RELIEF FEATURES OF THE THIRD ORDER Respectively.
  • 9.
    RELIEF FEATURES OFTHE FIRST ORDER On the smallst scale and covering the largest area is the ‘world geomorphology’. which includes consideration of continents and ocean basins consideration and interpretation of worldwide erosion surfaces requires the analysis of the characteristics and evolution of continents and ocean basins. Eg:plate tectonics help in understanding the origin of continents and ocean basins.
  • 10.
    RELIEF FEATURES OFTHE SECOND ORDER The structural forms developed over a continent part thereof as mountains,plateaus,lakes,faults,rift valleys etc. constitute the category of relief features of the second order. These are also known as “constructional landforms”.
  • 11.
    RELIEF FEATURES OFTHE THIRD ORDER Micro –level landforms developed on second order relief features by exogenic denudational processes originating from the atmosphere are included in this category. these landforms may be erosional(glacial valleys,river valley,karst valley etc) and depositional (drumlins,flood plains,inselbergs etc) and sometimes minor tectonics features(by endogenetic forces).
  • 12.