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DavidMP1. A user sandbox is a subpage of the user's
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This page is on thin-skinned deformation which is when only the top layers of rock deform but the basement does not.
1c
Another figure showing a cross section of how the upper rock deform while the basement stays the same would be useful to this article.
1d
The grammer and writing are good but the article is fairly short and could go into more detail about how stacks and other structures form as a result of this deformation.
1e
The photo is appropriate to the article but it would be better to have a cross section to show how the layers deform.
This page is on geologic folds which are often a byproduct of thin-skinned deformation.
3c
More could probably be added to explain the Mechanics of folds
3d
The written part of this page is of sufficient length to describe the subject and is well written.
3e
The visual part of this page is very good with many different graphics and not much to improve upon but it could also use a diagram showing how types stress can lead to folding.
Part 2
A
The topic I would like to make a page for is thick-skinned deformation, what it means, and how it differs from thin-skinned deformation.
B
The
current article on this topic is very small and there is much more that can be said about it. Thick-skinned deformation frequently occurs during continental collisions and other mountain building events and models for it can explain many surface features of the earth.
C
The page would start with a basic explanation of thick-skinned deformation and its differences from thin-skinned deformation, then talk about the types of processes that cause it and where they occur. The page would include a description of the type of structures that this type of deformation can form. The figure would be a basic drawing of the process of two plates colliding or the rise of plutonic bodies causing crustal deformation including the basement rock.
This is the user
sandbox of
DavidMP1. A user sandbox is a subpage of the user's
user page. It serves as a testing spot and page development space for the user and is not an encyclopedia article. Create or edit your own sandbox
here.
Finished writing a draft article? Are you ready to request review of it by an experienced editor for possible inclusion in Wikipedia? Submit your draft for review!
This page is on thin-skinned deformation which is when only the top layers of rock deform but the basement does not.
1c
Another figure showing a cross section of how the upper rock deform while the basement stays the same would be useful to this article.
1d
The grammer and writing are good but the article is fairly short and could go into more detail about how stacks and other structures form as a result of this deformation.
1e
The photo is appropriate to the article but it would be better to have a cross section to show how the layers deform.
This page is on geologic folds which are often a byproduct of thin-skinned deformation.
3c
More could probably be added to explain the Mechanics of folds
3d
The written part of this page is of sufficient length to describe the subject and is well written.
3e
The visual part of this page is very good with many different graphics and not much to improve upon but it could also use a diagram showing how types stress can lead to folding.
Part 2
A
The topic I would like to make a page for is thick-skinned deformation, what it means, and how it differs from thin-skinned deformation.
B
The
current article on this topic is very small and there is much more that can be said about it. Thick-skinned deformation frequently occurs during continental collisions and other mountain building events and models for it can explain many surface features of the earth.
C
The page would start with a basic explanation of thick-skinned deformation and its differences from thin-skinned deformation, then talk about the types of processes that cause it and where they occur. The page would include a description of the type of structures that this type of deformation can form. The figure would be a basic drawing of the process of two plates colliding or the rise of plutonic bodies causing crustal deformation including the basement rock.