Notice: Function _load_textdomain_just_in_time was called incorrectly. Translation loading for the search-in-place domain was triggered too early. This is usually an indicator for some code in the plugin or theme running too early. Translations should be loaded at the init action or later. Please see Debugging in WordPress for more information. (This message was added in version 6.7.0.) in /usr/www/users/mywaecf/KEYPOINT/wp-includes/functions.php on line 6121

Warning: session_start(): Cannot start session when headers already sent in /usr/www/users/mywaecf/KEYPOINT/wp-content/plugins/secure-copy-content-protection/public/class-secure-copy-content-protection-public.php on line 1000

Warning: Cannot modify header information - headers already sent by (output started at /usr/www/users/mywaecf/KEYPOINT/wp-includes/functions.php:6121) in /usr/www/users/mywaecf/KEYPOINT/wp-content/plugins/docket-cache/includes/src/Plugin.php on line 1186

Warning: Cannot modify header information - headers already sent by (output started at /usr/www/users/mywaecf/KEYPOINT/wp-includes/functions.php:6121) in /usr/www/users/mywaecf/KEYPOINT/wp-content/plugins/docket-cache/includes/src/Tweaks.php on line 453
Residual Mountains — Geography Keypoint

Residual Mountains

RESIDUAL MOUNTAINS are Mountains that evolve when the general level Of the land has been lowered by the agents of denudation leaving the more resistant areas to remain.

A good example of Residual Mountain is Mt. Monadnock in U.S.A., Highlands of Scotland, the Deccan plateau, the ldanre hills etc.

Agents of denudation form Residual Mountains from old fold, block or volcanic mountains. They may also come up from plateaux as hills and valleys that have been dissected by rivers.

Leave a Comment

not allowed!