Make eBroadcast my Homepage | Contact Us   Return To The Main eBroadcast Homepage
Australia
Web Guide Search
Australia
Welcome It's
Australia
Australia
Web Guide: Encyclopedia
EBroadcast Australia
Powered by Wikipedia
Contents

Mountain

Redirected from Hill

A mountain is a landform that extends above the surrounding terrain[?] in a limited area. A mountain is generally much higher and steeper than a hill, but there is considerable overlap, and usage often depends on local custom; see also Dune.

A mountain is usually produced by the movement of lithospheric plates, either orogenic movement[?] or epeirogenic movement[?]. The compressional forces, isostatic uplift and intrusion of igneous matter forces surface rock upwards, creating a landform higher than the surrounding features. The height of the feature makes it either a hill or, if higher and steeper, a mountain. The absolute heights of features termed mountains and hills vary greatly according to an area's topography. The major mountains tend to occur in long linear arcs, indicating tectonic plate boundaries and activity. Mountain creation tends to occur in discrete periods, referred to as orogenies (orogeny). Two types of mountain are formed depending on how the rock reacts to the tectonic forces - block mountains or fold mountains.

Some isolated mountains were produced by volcanoes, including many apparently small islands that reach a great height above the ocean floor.

Block mountains are created when large areas are widely broken up by faults creating large vertical displacements. The uplifted blocks are block mountains or horsts[?]. The intervening dropped blocks are termed graben[?], these can be small or form extensive rift valley systems. This form of landscape can be seen in East Africa, the Vosges, the Basin and Range province of Western North America and the Rhine valley.

Where rock does not fault it folds, either symmetrically or asymmetrically. The upfolds are anticlines and the downfolds are synclines, in asymmetric folding there may also be recumbent and overturned folds. The Jura mountains are an example of folding. Over time erosion can bring about an inversion of relief, the soft upthrust rock is worn away so the anticlines are actually lower than the tougher rock of the synclines.

The highest mountain on Earth is Mount Everest, set in the world's most significant mountain range, the Himalayas. Another contender for this title is Mauna Loa, which stands taller than Mount Everest when measured from its base on the ocean floor but not in terms of summit altitude. The tallest mountain in the solar system is Olympus Mons, located on Mars.

Some mountains are very difficult to climb, and offer spectacular views. Some people therefore enjoy the sport of mountaineering. Mountains are also the site for the sport of downhill skiing.

A popular form of playing at the beach is making a sand "mountain".

See also: List of mountains, Mountain range, List of mountain ranges

Elsewhere
EBroadcast Australia
Search engine
Web directory

CONTENTS:
A
B
C
D
E
F
G
H
I
J
K
L
M
N
O
P
Q
R
S
T
U
V
W
X
Y
Z

Australia
eBroadcast Australia
Australia © 06 eBroadcast Australia | About eBroadcast | Legal Notices | Privacy Policy | Contact Us    Return To The Main eBroadcast Homepage