My ten stages of spit are formed by a long narrow beach and a shingle attached to the end1. 2. An example of a spit is in devon bay. England and due to prevailing wind brings rainfull and bfings chemicial weathering and brings a most commond direct threat 3. Due to the estuary the deposits melt and the longshore drift carries the material and this is the beginning of a formation of a spit4. Over time the spi will become longer and longer
The water behing the spit is helterd and has low energy , because of the water behind the spit and having the low enery the materials deposits and longshore drifts will cary a sediment to allow the swash to say at an angle and the back swash or back wash to stay at an agle to a right.
N another thing when the material deposits a sal,arsh is formed , and finally at the top of the water the spit will stop rainfull drom carrying into a curve from a chamge of direbtion
Wait a minute, this is for GCSE level? I am in grade 8 and this is too little to explain anything that I have learned. In this grade, I have learned way more than this.
this is basic stuff you learn earlier on in school - its a very small part of gcse geography but you need to know the basics before you can move on lol
I’m in class watching this, this is very useful
I literally know all of this it is just that i am scared for the real exams
same!!!
this is savingmy life thanks sm
this is quite informative thnx!
My ten stages of spit are formed by a long narrow beach and a shingle attached to the end1. 2. An example of a spit is in devon bay. England and due to prevailing wind brings rainfull and bfings chemicial weathering and brings a most commond direct threat 3. Due to the estuary the deposits melt and the longshore drift carries the material and this is the beginning of a formation of a spit4. Over time the spi will become longer and longer
Amazing
Thank you very much
The water behing the spit is helterd and has low energy , because of the water behind the spit and having the low enery the materials deposits and longshore drifts will cary a sediment to allow the swash to say at an angle and the back swash or back wash to stay at an agle to a right.
Yep swash is at an angle backwash or back swash is at a straight angle to a right
N another thing when the material deposits a sal,arsh is formed , and finally at the top of the water the spit will stop rainfull drom carrying into a curve from a chamge of direbtion
Shut the fuck up
How do i copy this video onto my powerpoint to show my class??
+Skilled Gamer01 I would put in a hyperlink
When wind changes direction it can curve at any angle okay
Other wise it will be a bar and the bar is where two headland creats a lagoon to cut it self
Me importa demasiado
A tombol os connected to an island
Wait a minute, this is for GCSE level? I am in grade 8 and this is too little to explain anything that I have learned. In this grade, I have learned way more than this.
Lol y10 for me
this is basic stuff you learn earlier on in school - its a very small part of gcse geography but you need to know the basics before you can move on lol
Same :P
Ohh yea i commented on dat
The spit cannot reach the river estaury
The spit will become longer and longer