1 |
Soils between present flood plains and old bar areas are known as: |
Khaddar soils
Bangarsoil
Alluvialsoil
Aridisolsoil
|
2 |
Bangarsoil of regions of doabs is: |
Old, rivers transported soil
Fresh alluvialsoil
Recent age transported soil
Localsoil
|
3 |
Soils of high bar areas is called - scalloped interfluvies: |
Bangarsoil
Khaddarsoil
Entisolssoil
Inceptisolssoil
|
4 |
In Pakistan, river Sindh plain is composed of: |
Alluvial soil
Clayeysoil
Sandysoil
Localsoil
|
5 |
Soil possessing pH value from 7 - 11 is called: |
Alkaline soil
Acidicsoil
Neutralsoil
Fertilesoil
|
6 |
Soil with pH value, 4 - 7 is called: |
Acidic soil
Basicsoil
Neutralsoil
Alkalinesoil
|
7 |
Mixture of sandy and clayey soil is called: |
Loamy soil
Clayey soil
Sandy soil
Silty soil
|
8 |
In Pakistan, Bela forests are found: |
Along the banks of the major rivers
In mountain areas
Along the coast of the sea
In the areas of Pakistan
|
9 |
Pakistan's three percent mangrove forests are found: |
Along the Sindh coast
Along the Baluchistan coast
In the N.W.F province
In the southern Punjab
|
10 |
Mangrove forests along the coast of Sindh are: |
97% of the total mangrove forests
50% of the total mangrove forests
Only 10% of the total mangrove forests
Not found
|
11 |
In Pakistan, mangrove forests are found: |
In the Punjab province
Along the Sindh coastal area
Nowhere in the country
In KPK at some places
|
12 |
Pakistan's those area, where rainfall is upto 10 inches: |
Natural vegetation is grass
Natural vegetation is not grass
Xerophytes vegetation is found
Forest does not exist
|
13 |
Tropical deciduous plain forests are found in: |
Plain area
The flood plains & banks of the major rivers
Lower plain area
Bar region of upper ludus
|
14 |
In Pakistan, deciduous forests are found in mountainous region up to: |
Altitude of 3,000 - 5,000 feet
Does not exists
At large area
At very small area
|
15 |
In Pakistan, Deodar, Kail, Supruce and Fur forests are: |
Found everywhere
Found at some places
In north and north-eastern mountainous region
Found nowhere
|