The class of 4E5'10

Th


Individually,we are one drop
Together,we are an ocean

Together, we can.

Hello there, we are a bunch of very
diligent + innocent + adorable kids students of 4E5'10.

We love to laugh,
we love to take nutritious brain food in class
Basically, we are like that because we are from 4 E 5 .
and yes,we crap alot as well.

We are under the command
of MR TAN YS and MDM NOREHA

For any queries,
feel free to type them out in the comment box.

Have a nice day too !





Triple Maths Students

Agnes●Dawn●Eliza●Faiqah●Hadianti
Jane●Christina●JingShi●Jojo●Lydia
Michelle●Natalie●Afiqah●Nurain●Atikah
JiaQian●YuYu●Shilpa●Syarifah●SiewHuey
Jeannie●JiaXi

Asyraf●WeeKiat●ZhiRan●Sherman●Cornelius
Danny●Eric●Jeremy●Jerome●Alex
Aaron●Harold●Haziq●BangXiang●KerFang
Terence●Julian●Xavier

4 E 5 Babies

January

4/1 - Jeannie
23/1 BangXiang
25/1 - Michelle

February

2/2 - JingShi

March

1/3 - WeeKiat
15/3 - Jojo
18/3 - Alex

 April

4/4 - Jane
10/4 - Xavier
28/4 - Asyraf

May

27/5 - Afiqah
31/5 - Christina

June

16/6 - Natalie
17/6 - Syarifah
27/6 - Shilpa
28/6 - Cornelius
30/6 - Terence

July

25/7 - Dawn
30/7 - Faiqah
31/7 - Agnes
31/7 - Haziq

August

11/8 - Julian
15/8 - Nurain
22/8 - Hadianti
25/8 - Harold

September

7/9 - Aaron
27/9 - Lydia
29/9 - Eric

October

1/10 - Atikah
13/10 - ZhiRan
18/10 - YuYu

November

08/11 - KerFang
10/11 - JiaXi
11/11 - Jeremy
12/11 - JiaQian
14/11 - Sherman
15/11 - SiewHuey
19/11 - Jerome
21/11 - Danny

December

12/12 - Eliza

Teachers
Form teacher :
Mr Tan Yim Siong Gif Cute Heart Pictures, Images and Photos

 Form tutor :
Mdm Noreha

 English :
Ms Chong
Ms Liu
Mdm Noreha
Ms Wani

Social Studies :
Mdm Noreen

A/E maths :
Mr Tan Yim Siong

Physics :
Ms Tay

Chemistry :
Ms Chan

Geog Elective :
Mrs Lee

History Elective:
Ms Cloven Ong Mei Zhi

MT Chinese :
Mr Ng/Ms Yap

MT Malay :
Mdm Alimah Lob

about this blog
This blog is not offically opened by
MR OBAMA to accomodate 4e5's mindless musings
and daily rantings.

Do enjoy your stay here,
and don't take what's not yours!


Anonymous tags
will NOT be entertained :)

Links



March 2009 April 2009 May 2009 June 2009 July 2009 August 2009 September 2009 October 2009 November 2009 March 2010


Thanks,

Basecodes Designer
Monday, April 20, 2009,
♥ 7:03 PM

Geography notes


Longshore Drift
Where waves approach the coastline at an angle, when they break their swash pushes beach material up the beach at the same angle. The backwash then drags the material down the beach perpendicular (at a 90º angle) to the shore, following the line of the steepest gradient. This produces a zig-zag movement of sediment along the beach known as longshore drift. Largest beach sediment is found updrift, and the smallest material, which is more easily moved, downdrift.
if you can't get to the website click the link in this page :)

Wave Refraction and Coastal Defences
Friction with the sea bed as waves approach the shore causes the wave front to become distorted or refracted as velocity is reduced. The image below shows how the refracted wave becomes increasingly parallel to the shoreline. Waves in the middle of the bay, where the water is deeper, do not lose velocity as rapidly. Since the paths of the waves in the bay are diverging or spreading out, wave energy is much reduced, allowing deposition to occur.


The coastal defence rock islet in the diagram below absorbs wave energy but interferes with the pattern of waves. The waves refract round the islet, with wave fronts crossing each other in the lee of the island. This would leave some parts of the beach behind the islet with waves approaching parallel to the shore and others with waves approaching at an angle. Waves breaking at an angle on some areas of the the beach would thus lead to the removal of sediment by longshore drift.


For headlands and bays
Formation of headlands and bays:
The coastline consisted of parallel bands of hard and soft rock which were perpendicular to the sea. As a result of differential erosion, the bands of soft rock were eroded much more quickly than the bands of resistant rock to form BAYS ans HEADLANDS. The headlands will be eroded back as a result of wave refraction. Caves, arches, stacks, and stumps will form which will eventually erode away. The bays will advance as deposition will take place at their heads to form BAY-HEAD BEACHES. Eventually the coastline will become straight again and the whole process of differential erosion will resume again to result in an irregular coastline.



For further information about caves, arches,stacks,stumps,
refer to the useful link :
All the best for the GG test tomorrow!!! :)


♥Christina
To accomplish great things,
we must not only act, but also dream; not only plan, but also believe.
:)