User talk:EHitchcock

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Welcome![edit]

Hello, EHitchcock, and welcome to Wikipedia! Thank you for your contributions. I hope you like the place and decide to stay. Here are a few links to pages you might find helpful:

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Hello EHitchcock.

I am your course online ambassador. This means that I will try to assist you to get your article into Wikipedia, using the style and techniques required here. I am a volunteer working from Australia, so my timezone overlaps with yours quite a bit. You are welcome to ask me questions on my talk page or to use email on this screen: Special:EmailUser/Graeme_Bartlett.

I am looking forward to your new article and your improvements to Wikipedia. Graeme Bartlett (talk) 06:15, 21 September 2016 (UTC)[reply]

Referencing[edit]

Hello Elizabeth. I have been looking at your sandbox. I notice you have numbers in parenthesis that look like references, but there is no bibliography or reference section yet to see what they mean. You may wish to read Help:Referencing for beginners to learn how to add nice footnotes here. If you can get hold of a doi for a journal article you use, it makes it very easy to fill the reference out. Graeme Bartlett (talk) 11:00, 12 October 2016 (UTC)[reply]

Hello Graeme

https://en.wikipedia.org/wiki/User:EHitchcock/sandbox

This is the like to my page, although you obviously have already seen it but I was told to send it and don't want to miss out on marks for not sending it!

Thank you for saying about the referencing, I have looked at that in class today and am just about to start on sorting it now. Those links will be really helpful - thank you. Next challenge will be putting up my Inkscape diagrams so I may have a few questions heading your way! Ill do my best to work it out first though.

Thanks, Beth

Review from Jeffrey[edit]

Hi Beth this is Jeffrey from regional geology class. Your page is quite interesting and organized but it may need a few amendments, apart from obviously filling in the empty sections and doing a spelling check (ophiolite is spelled wrongly in the overview section while magmatism is spelled as magnetism in Mesozoic subduction section, which makes a huge difference:p).

1) perhaps links to other wikipedia pages would help the readers to understand better, as not everyone has the basic knowledge to some of the geographical and geological terms here, such as kalimanton (i would not know where that is without looking it up in wiki or google) , ophiolite, tonalite, and maybe also Borneo to show the approximate current geographical position of the place (or maybe you can show that by creating a small inset diagram in your second diagram)

2) it seems that the sub-section 'Subduction Model for South China Sea Spreading' is one of the 3 models for Cenozoic south china sea extension. Therefore, i think it should be placed under the section 'Cenozoic south china sea extension' instead of 'Late Ceneozoic Magmatism and the Mount Kinabalu Intrusion'

3) the diagrams can be improved by more labeling and perhaps some more description in the caption. For example, the red line is not defined for in your second diagram (I'm guessing that it means to be the line of magmatic arc), and the meaning of blue area in your third diagram is also unknown. The subduction zone is also poorly mapped in the 2nd model of the third diagram, particularly the subduction boundary along the proto-south china sea.

4) I would suggest a comparison between the 3 models for south china sea extension, both the features, mechanisms and plausibility.

Cheers! Jeffrey — Preceding unsigned comment added by 2001:CE0:2207:8802:2558:2E67:2A57:6F24 (talk) 16:35, 17 October 2016 (UTC)[reply]

Images[edit]

I notice that you have uploaded some images from a thesis. The one at http://etheses.dur.ac.uk/9450/1/Complete_Thesis_-_Post-Viva_-_Mt_Kinabalu_-_Alex_Burton-Johnson_2013.pdf. The thesis actually says:"The copyright of this thesis rests with the author. No quotation from it should be published without the author’s prior written consent and information derived from it should be acknowledged" and also "The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-proit purposes provided that..". Where do you have evidence that the images are in the public domain released by BURTON-JOHNSON, ALEXANDER? It dfoes not say that in the thesis. In the UK where this came from, I don't even think it is legally possible to release into the public domain. That is why there is a CC-Zero license. Graeme Bartlett (talk) 10:06, 19 October 2016 (UTC)[reply]

Saving[edit]

Hi Beth,

it is a few hours since you had your problem. I suggest that you should just wait a bit and try save again. If needed copy and paste your work into an off-line file eg notepad and save with utf-8. Then later past your work back in when you can edit. I note that you have not managed to save after posting on my talk page. You may have logged out before you manage to save. That would explain the edits from 147.8.234.99 on your sandbox. You should log on again. Graeme Bartlett (talk) 07:53, 15 November 2016 (UTC)[reply]

Thanks Graeme,

I have now made the updates that I want and would like to make it live. I can't seem to find where to do this. Could you please help. Thank you. Beth

File permission problem with File:Extrusion Model for the cenozoic spreading of the South China Sea.pdf[edit]

Thanks for uploading File:Extrusion Model for the cenozoic spreading of the South China Sea.pdf. I noticed that while you provided a valid copyright licensing tag, there is no proof that the creator of the file has agreed to release it under the given license.

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File permission problem with File:300 Ma map of world. Tectonic setting.pdf[edit]

Thanks for uploading File:300 Ma map of world. Tectonic setting.pdf. I noticed that while you provided a valid copyright licensing tag, there is no proof that the creator of the file has agreed to release it under the given license.

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DYK for Geological history of Borneo[edit]

On 17 January 2017, Did you know was updated with a fact from the article Geological history of Borneo, which you recently created, substantially expanded, or brought to good article status. The fact was ... that the Crocker Fan in Borneo has the largest volume of any Paleogene deep marine sediment in a single basin in southeast Asia? The nomination discussion and review may be seen at Template:Did you know nominations/Geological history of Borneo. You are welcome to check how many page hits the article got while on the front page (here's how, Geological history of Borneo), and it may be added to the statistics page if the total is over 5,000. Finally, if you know of an interesting fact from another recently created article, then please feel free to suggest it on the Did you know talk page.

Cas Liber (talk · contribs) 12:02, 17 January 2017 (UTC)[reply]

A tag has been placed on File:Borneo map of location in South East Asia inclusion india.pdf requesting that it be speedily deleted from Wikipedia. This has been done under section F10 of the criteria for speedy deletion, because it is a file that is not an image, sound file or video clip (e.g. a Word document or PDF file) that has no encyclopedic use.

If you think this page should not be deleted for this reason, you may contest the nomination by visiting the page and clicking the button labelled "Contest this speedy deletion". This will give you the opportunity to explain why you believe the page should not be deleted. However, be aware that once a page is tagged for speedy deletion, it may be deleted without delay. Please do not remove the speedy deletion tag from the page yourself, but do not hesitate to add information in line with Wikipedia's policies and guidelines. Pkbwcgs (talk) 15:53, 16 April 2018 (UTC)[reply]

A tag has been placed on File:Cenozoic subduction model to describe the spreading of the south china sea.pdf requesting that it be speedily deleted from Wikipedia. This has been done under section F10 of the criteria for speedy deletion, because it is a file that is not an image, sound file or video clip (e.g. a Word document or PDF file) that has no encyclopedic use.

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A tag has been placed on File:Continental Rifting Basin Model for the spreading of the south china sea.pdf requesting that it be speedily deleted from Wikipedia. This has been done under section F10 of the criteria for speedy deletion, because it is a file that is not an image, sound file or video clip (e.g. a Word document or PDF file) that has no encyclopedic use.

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A tag has been placed on File:3 models for spreading of the south china sea.png requesting that it be speedily deleted from Wikipedia. This has been done under section F3 of the criteria for speedy deletion, because it is a file licensed as "for non-commercial use only", "no derivative use", "for Wikipedia use only", or "used with permission"; and it has not been shown to comply with the limited standards for the use of non-free content. If you agree with the deletion, there is no need to do anything. If, however, you believe that this image may be retained on Wikipedia under one of the permitted conditions then:

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A tag has been placed on File:Extrusion model for south china sea spreading during the cenozoic.pdf requesting that it be speedily deleted from Wikipedia. This has been done under section F10 of the criteria for speedy deletion, because it is a file that is not an image, sound file or video clip (e.g. a Word document or PDF file) that has no encyclopedic use.

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A tag has been placed on File:Map of Borneo, SE Asia. Showing ophiolite, magmatism and sedimentation.pdf requesting that it be speedily deleted from Wikipedia. This has been done under section F10 of the criteria for speedy deletion, because it is a file that is not an image, sound file or video clip (e.g. a Word document or PDF file) that has no encyclopedic use.

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A tag has been placed on File:Mesozoic subduction and the plates involved in south east asia.pdf requesting that it be speedily deleted from Wikipedia. This has been done under section F10 of the criteria for speedy deletion, because it is a file that is not an image, sound file or video clip (e.g. a Word document or PDF file) that has no encyclopedic use.

If you think this page should not be deleted for this reason, you may contest the nomination by visiting the page and clicking the button labelled "Contest this speedy deletion". This will give you the opportunity to explain why you believe the page should not be deleted. However, be aware that once a page is tagged for speedy deletion, it may be deleted without delay. Please do not remove the speedy deletion tag from the page yourself, but do not hesitate to add information in line with Wikipedia's policies and guidelines. Pkbwcgs (talk) 12:39, 22 August 2018 (UTC)[reply]

Notice

The file File:Regional map of SE asia with Borneo Highlighted.pdf has been proposed for deletion because of the following concern:

Converted to SVG and uploaded at File:Regional map of SE Asia with Borneo Highlighted.svg

While all constructive contributions to Wikipedia are appreciated, pages may be deleted for any of several reasons.

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PDF uploads[edit]

FYI, though Wikipedia does permit PDF uploads and they will usually be rendered correctly if they are image-based PDFs, a native image format is preferable. If it's a vector-based image, SVG is the most preferred option. If it's a non-vector chart, logo, or map, then PNG is preferred. If it's a photo, JPEG is the best option. I converted one of your PDFs to SVG. RHaworth (talk · contribs) converted one to PNG. --B (talk) 12:14, 24 August 2018 (UTC)[reply]

File permission problem with File:Western Pacific subduction during the Mesozoic - active margin.png[edit]

Thanks for uploading File:Western Pacific subduction during the Mesozoic - active margin.png. I noticed that while you provided a valid copyright licensing tag, there is no proof that the creator of the file has agreed to release it under the given license.

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