Morphology and Morphometry watershed is a specific description of the watershed that was characterized by parameters related with: broad, shape, orientation, altitude, slope, flow patterns, river gradient, and the River’s density. This study aims to obtain data Morphology and Morphometry watershed conditions. Steps of this study were (1) identified criteria of morphology and morphometry watershed, (2) overlay watershed parameters. The results of this study were (1) Way Mesuji sub watershed is dominated by an elongated shape. This is caused the value of each Circularity Ratio Way Mesuji sub-watershed  less than 0.5; (2) Sub-watershed Slope is dominated by flat and ramps.This will result a slow velocity river stream; (3) region  altitude ...
Bengawan Solo river flow changes is estimated to occur about 2 or at least a million years ago. The ...
Bengawan Solo river flow changes is estimated to occur about 2 or at least a million years ago. The ...
Bengawan Solo river flow changes is estimated to occur about 2 or at least a million years ago. The ...
Morphometric analysis in a watershed is a requirement in analyzing hydrological conditions in a wate...
Morphometric analysis in a watershed is a requirement in analyzing hydrological conditions in a wate...
Upper Citarik River is the Inter Mountainous Valley of Volcanic Denudational Landform in the eastern...
The low location of the Banjar district land from the sea surface causes the flow of water on the so...
The low location of the Banjar district land from the sea surface causes the flow of water on the so...
The low location of the Banjar district land from the sea surface causes the flow of water on the so...
The low location of the Banjar district land from the sea surface causes the flow of water on the so...
Until today, the development of synthetic unit hydrograph model is still based on morphometry charac...
Until today, the development of synthetic unit hydrograph model is still based on morphometry charac...
Padang City is the capital of West Sumatra Province. This city has several rivers, each of which is ...
This paper presents the identification, assessment and visualization of physical, topographic, morph...
This paper presents the identification, assessment and visualization of physical, topographic, morph...
Bengawan Solo river flow changes is estimated to occur about 2 or at least a million years ago. The ...
Bengawan Solo river flow changes is estimated to occur about 2 or at least a million years ago. The ...
Bengawan Solo river flow changes is estimated to occur about 2 or at least a million years ago. The ...
Morphometric analysis in a watershed is a requirement in analyzing hydrological conditions in a wate...
Morphometric analysis in a watershed is a requirement in analyzing hydrological conditions in a wate...
Upper Citarik River is the Inter Mountainous Valley of Volcanic Denudational Landform in the eastern...
The low location of the Banjar district land from the sea surface causes the flow of water on the so...
The low location of the Banjar district land from the sea surface causes the flow of water on the so...
The low location of the Banjar district land from the sea surface causes the flow of water on the so...
The low location of the Banjar district land from the sea surface causes the flow of water on the so...
Until today, the development of synthetic unit hydrograph model is still based on morphometry charac...
Until today, the development of synthetic unit hydrograph model is still based on morphometry charac...
Padang City is the capital of West Sumatra Province. This city has several rivers, each of which is ...
This paper presents the identification, assessment and visualization of physical, topographic, morph...
This paper presents the identification, assessment and visualization of physical, topographic, morph...
Bengawan Solo river flow changes is estimated to occur about 2 or at least a million years ago. The ...
Bengawan Solo river flow changes is estimated to occur about 2 or at least a million years ago. The ...
Bengawan Solo river flow changes is estimated to occur about 2 or at least a million years ago. The ...