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Sri Aman, Sarawak, Malaysia
-Leo- -expansive -generous and caring -flamboyant

Sunday 17 April 2011

Hotel in Sri Aman

Hoover Hotel
139, Jalan Club, 95000 Sri Aman.
Tel : 083-321985/321987/321989
Fax : 083-321520

Mega Inn
Lot 1704-1706, Jalan Durian,
95000 Sri Aman.
Tel : 083-326998/326361/326360
Fax : 083-326362

Tiara Inn
Lot 436, Jalan Council Block 3, STD PO BOX 365,95000 Sri Aman.
Tel : 083-325832/325834/325835
Fax : 083-321520

Crystal Inn
Lot 106, Block 2, Jalan Club, 95000 Sri Aman.
Tel : 083-326822/326762/326862
Faks : 083-321520

Theatre Inn
Lot 106, Block 2 Jalan Club, 95000 Sri Aman.
Tel : 083-323122
Faks : 083-323211

Taiwan / Alishan Hotel
No. 123, Council Road, 95000 Sri Aman.
Tel : 083-322497
Fax : 083-321167

Good View Inn
Lot 1907/1908, Jalan Serian Simanggang, 95000 Sri Aman.
Tel : 019-8281257

Champion Inn
Jalan Sim Kim, Sri Aman Bazaar, 95000 Sri Aman.
Tel : 083-320142
Fax : 083-320752

Regent Inn
Lot 1856-1858
Jalan Sabu, 95000 Sri Aman.
Tel : 083-325857
Fax : 083-327857

Mei Xing Inn
1st & 3rd Floor, Jalan main Bazaar,
95000 Sri Aman.
Tel : 083-323511
Fax : 083-323522

Monday 4 April 2011

How is Soil Formed?

    There are thousands of different soils throughout the world. Soils are formed through a combination of five important factors.


      Parent Material 
      - Earthy materials, both mineral and organic. Parent material can be a volcanic deposit such as ash; it can be a sediment that has been transported and deposited by wind or water; or it can be a deposit left by glaciers.
        Climate 
        - Parent material is broken down into finer particles by a process called weathering, which is controlled by the climate of a given location. Temperature and water are major climatic forces that influence weathering.
          Living Organisms
           - Both plants and animals help to create soils. As they die, plants and animals add organic matter to weathered parent material to help form subsoil and topsoil. As animals dig through the soil, they break it up, permitting more are and water to enter.
            Topography
             - Topography is the hilliness, flatness, or amount of slope of the land.
              Time 
              - The age of a soil must be considered in thousands and even millions of years since it may take hundreds of years for these factors to form one inch of soil from parent material.

            Sunday 17 April 2011

            Hotel in Sri Aman

            Hoover Hotel
            139, Jalan Club, 95000 Sri Aman.
            Tel : 083-321985/321987/321989
            Fax : 083-321520

            Mega Inn
            Lot 1704-1706, Jalan Durian,
            95000 Sri Aman.
            Tel : 083-326998/326361/326360
            Fax : 083-326362

            Tiara Inn
            Lot 436, Jalan Council Block 3, STD PO BOX 365,95000 Sri Aman.
            Tel : 083-325832/325834/325835
            Fax : 083-321520

            Crystal Inn
            Lot 106, Block 2, Jalan Club, 95000 Sri Aman.
            Tel : 083-326822/326762/326862
            Faks : 083-321520

            Theatre Inn
            Lot 106, Block 2 Jalan Club, 95000 Sri Aman.
            Tel : 083-323122
            Faks : 083-323211

            Taiwan / Alishan Hotel
            No. 123, Council Road, 95000 Sri Aman.
            Tel : 083-322497
            Fax : 083-321167

            Good View Inn
            Lot 1907/1908, Jalan Serian Simanggang, 95000 Sri Aman.
            Tel : 019-8281257

            Champion Inn
            Jalan Sim Kim, Sri Aman Bazaar, 95000 Sri Aman.
            Tel : 083-320142
            Fax : 083-320752

            Regent Inn
            Lot 1856-1858
            Jalan Sabu, 95000 Sri Aman.
            Tel : 083-325857
            Fax : 083-327857

            Mei Xing Inn
            1st & 3rd Floor, Jalan main Bazaar,
            95000 Sri Aman.
            Tel : 083-323511
            Fax : 083-323522

            Monday 4 April 2011

            How is Soil Formed?

              There are thousands of different soils throughout the world. Soils are formed through a combination of five important factors.


                Parent Material 
                - Earthy materials, both mineral and organic. Parent material can be a volcanic deposit such as ash; it can be a sediment that has been transported and deposited by wind or water; or it can be a deposit left by glaciers.
                  Climate 
                  - Parent material is broken down into finer particles by a process called weathering, which is controlled by the climate of a given location. Temperature and water are major climatic forces that influence weathering.
                    Living Organisms
                     - Both plants and animals help to create soils. As they die, plants and animals add organic matter to weathered parent material to help form subsoil and topsoil. As animals dig through the soil, they break it up, permitting more are and water to enter.
                      Topography
                       - Topography is the hilliness, flatness, or amount of slope of the land.
                        Time 
                        - The age of a soil must be considered in thousands and even millions of years since it may take hundreds of years for these factors to form one inch of soil from parent material.