the well sorted is on the left & the poorly sorted is on the right .. It all depends on the arrangement and size of the rocks
Well it depends on whether you like teen romance or not. Most people would say Yes. It is aimed to please people with a small IQ
well nobody's perfect! Miley got MAJOR ugly breakouts but she went to a specialist to get is sorted out
Camping, lack of comfort and the greatly reduced number of meals.
Shammurat and Semiramis denote the same person according to the available sources given in the related web site. The spellings differ slightly. In some places Shammurat is given as Sammuramat which is an Assyrian name used even presently. Semiramis is is used in Greek and Arabic as well. If any one knows about please contribute
There is alliteration and assonance, but since centering consonants differ, I would speak of consonance because, well the term for word initial consonance is alliteration but then again, I would say it's wrong either
A well sorted soil has particles which are all a similar size, a well graded soil would be classified as poorly graded. Whereas a poorly sorted soil has a wide range of particle sizes and is classified as well graded. On a particle size distribution a well sorted soil gives a steep gradient.
sorting is the tendency for currents of air or water to separate sediments according to size. sediments that can be sorted is sorted very poorly or somewhat between good and bad sorting. all the grains are rough in the well sorted sediments from the same sized and shape. many different size and shape sediments are sorted in the very poorly sediments category. the sorting of a result of change in the in speed of that agent that is moving the sediments.
Water transport generally results in the most well-sorted sediments, as the sorting of particles based on size occurs more efficiently in water compared to other transport media such as wind or ice. The constant movement and turbulence of water helps to separate particles by size, leading to well-sorted sediments.
poorly sorted = low porosity well sorted = high porosity
Sediments in outwash are typically well-sorted and composed of sand and gravel, deposited by meltwater streams flowing from glaciers. In contrast, sediments in moraines are unsorted and contain a mix of various sizes of rocks, debris, and till that has been directly deposited by the glacier. Outwash sediments are usually sorted by size and shape, while moraine sediments are unsorted and show a wider range of material types.
When all the particles in sediment are about the same size, the sediment is said to be well-sorted. Well-sorted sediments have particles that are uniform in size, typically due to a similar energy environment during deposition. This can indicate long transport distances or selective sorting processes.
Wave base is typically measured as the depth at which wave action is felt on the seafloor. This is commonly determined by the distance between the wave crest and the seafloor. One method is to analyze sediment samples to identify the depth at which there is a transition from well-sorted to poorly-sorted sediments, indicating the influence of wave energy.
A well-sorted sediment is composed of particles that are similar in size and shape. This indicates that the sediment has experienced minimal transport and disturbance, allowing particles of similar size to settle together. Well-sorted sediments typically have higher porosity and better sorting due to the similarity in particle size, making them easier to study and interpret.
Grain size and sorting are key indicators. Rocks formed in shallow water near shore tend to have larger, poorly sorted grains, reflecting the energy of the environment. In contrast, rocks formed in deep water tend to have smaller, well-sorted grains due to the quieter conditions.
The amount of uniformity in the size of rock or sediment particles is called "sorting." Sorting can range from well-sorted (similar-sized particles) to poorly sorted (a wide range of particle sizes).
When all the grains in a rock are roughly the same size, the rock is said to be well-sorted. This indicates that the grains were transported and deposited in a consistent manner, usually by wind or water, allowing them to settle according to size. Well-sorted rocks often have higher permeability and porosity compared to poorly sorted rocks.
Erosion can sort sediment based on size and weight. During erosion, heavier and larger particles settle faster than smaller and lighter particles. This results in the sorting of sediment by particle size, with larger particles typically being deposited first as the flow of water or wind decreases in speed.