© THEPUBLISHING.CO.UK

  •

    0 Using a small reference image – 1

    0.00 of 0 votes

    If preferred you can choose to have a small reference image at the head of your post by using an image 275px wide and 175px high (or in those proportions, i.e. 1.57:1). You can include white space around the image as is shown in the sample image above which is 138px wide x 88px high overall including white space to the side and bottom.

  •

    0 Using a small reference image – 2

    0.00 of 0 votes

    If preferred you can choose to have a small reference image at the head of your post by using an image 275px wide and 175px high (or in those proportions, i.e. 1.57:1). You can include white space around the image as is shown in the sample image above which is 137px wide x 87px high overall including white space to the (right) side and bottom. Just bear in mind that if you use a photograph or detailed graphic it will pixelate in the main categories window (as shown) as it tries to fill the 275px x 175px area.

  •

    0 Using no reference image at all

    0.00 of 0 votes

    If you prefer not to have a reference image at all just choose a very small white image file 1px wide x 1px high, to act as a spacer before your the start of your text content.

  •

    0 Add an image within the text content

    0.00 of 0 votes

    You can add images within text content by placing the cursor where you want the image to appear and then selecting the insert/edit image icon above. See below: Beaches are the result of wave action by which waves or currents move sand or other loose sediments of which the beach is made as these particles are held in suspension. Alternatively, sand may be moved by saltation (a bouncing movement of large particles). Beach materials come from erosion of rocks offshore, as well as from headland erosion and slumping producing deposits of scree. A coral reef offshore is a significant source of sand particles. Some species of fish that feed on algae attached to coral outcrops and rocks can create substantial quantities of sand particles over their lifetime as they nibble during feeding, digesting the organic matter, and discarding the rock and coral particles which pass through their digestive tracts. The composition of the beach depends upon the nature and quantity of sediments upstream of the beach, and the speed of flow and turbidity of water and wind. Sediments are moved by moving water and wind according to their particle size and state of compaction. Particles tend to settle and compact in still water. Once compacted, they are more resistant to erosion. Established vegetation (especially species with complex network root systems) will resist erosion by slowing the fluid flow at the surface layer. When affected by moving water or wind, particles that are eroded and held in suspension will increase the erosive power of the fluid that holds them by increasing the average density, viscosity, and volume of the moving fluid.

  •

    0 Add an image alongside text

    0.00 of 0 votes

    If you are an advanced user – or feeling "brave " – you can add an image alongside text content using a table as shown below (refer to the Simple Web Editor Manual). Beaches are the result of wave action by which waves or currents move sand or other loose sediments of which the beach is made as these particles are held in suspension. Alternatively, sand may be moved by saltation (a bouncing movement of large particles). Beach materials come from erosion of rocks offshore, as well as from headland erosion and slumping producing deposits of scree. A coral reef offshore is a significant source of sand particles. Some species of fish that feed on algae attached to coral outcrops and rocks can create substantial quantities of sand particles over their lifetime as they nibble during feeding, digesting the organic matter, and discarding the rock and coral particles which pass through their digestive tracts. The composition of the beach depends upon the nature and quantity of sediments upstream of the beach, and the speed of flow and turbidity of water and wind. Sediments are moved by moving water and wind according to their particle size and state of compaction. Particles tend to settle and compact in still water. Once compacted, they are more resistant to erosion. Established vegetation (especially species with complex network root systems) will resist erosion by slowing the fluid flow at the surface layer. When affected by moving water or wind, particles that are eroded and held in suspension will increase the erosive power of the fluid that holds them by increasing the average density, viscosity, and volume of the moving fluid.

You have full access to the “Source code” in the “Simple Web Editor” which means that you have the option to insert images into the text content including photos, illustrations and tables etc. The manual provides code examples which can easily be copied, modified and pasted into the “Source code” to suit whatever you wish to include in your page layouts.
The Books of Charles McHendrie
Some Page Options

© THEPUBLISHING.CO.UK

You have full access to the “Source code” in the “Simple Web Editor” which means that you have the option to insert images into the text content including photos, illustrations and tables etc. The manual provides code examples which can easily be copied, modified and pasted into the “Source code” to suit whatever you wish to include in your page layouts.
Some Sample Pages