What are the three main types of lipids

Three main lipids are triacylglycerols, phospholipids and sterols.

Explanation:

Lipids are important to play different roles in human body such as energy storehouse, important signaling molecules and structural components of cell membrane. These are belongs to organic compounds which are mostly insoluble in water.

Triacylglycerols: They are also called triglycerides. Naturally occurring triglycerides are present in many food items such as olive, corn, nuts, and avocados. Commonly triglycerides in our food is oils, and fat.

Phospholipids: They are present in both plants and animals, and water-soluble in nature. Phospholipids responsible for create a protective barrier around the body cells. They synthesized in the body for the formation of cell and organelle membranes.

Sterols: Cholesterol is the best example of sterol. The body produces most of the cholesterol and gets only small amount of cholesterol from the food. Cholesterol is necessary for the synthesis of vitamin D, bile salts, and sex hormones so, cholesterol is the main important component of the cell membrane.

from almost the creation of the first true maps of the earth, people started seeing how continents would be able to fit together.   in particular, people noticed that south america fits almost exactly into africa.

you should be aware that while world maps were around early in the 1600’s and better defined by the end of the 1700’s, those maps were not ‘public’ but were treated as state secrets.   and so it was not till much later that the broader ‘science’ community had access to good quality and accurate world maps.

get the whole story here…

it is now known that most of the major continental masses can be fit together in a jigsaw process.   in fact we now know that the continents were indeed once all joined together as one land mass – the supercontinent of pangaea.

if you look at most world maps you will ponder how this is evidence, as the continents really don’t appear to ‘fit’ together very well.   what you need to understand is that the vast majority of maps are drawn using a map projection that has the north and south poles (which are points) are a line the width of the map at the top and bottom.   this means that the map distorts the true shape of the earth’s land and oceans as you love closer to the poles.     some other map projections distort less, but have the map shape looking like segments of an orange.   see here for a range of map projections.   check out the way greenland changes size in each!

what is more remarkable, is the next piece of evidence when added to the shape of continents.

location of mountains and fossils

what is remarkable, when you reassemble all the continents together, the ancient mountain ranges (many now eroded to their cores) and the location of rock types and fossils all match up.

c. earths continental crust is thicker than its lithosphere.

because, the lithosphere is the outermost layer of the earth/ 100 km thick and is defined by its machanical properties.the lithosphere contains oceanic and continental crust that varies in age and thickness across locations and geologic time. the lithosphere is the coolest layer of the earth in terms of temperature. the term lithosphere should not be confused with the use of "geosphere" which is used to indicate all of earth systems, including the atmosphere, hydrosphere   and biosphere. the surface of the earth can be divided into the continental crust and the oceanic crust.   the continental crust is made mostly of granite while the oceanic crust is made of basalt. the average thickness of the continental crust is 25 miles and the average thickness of the oceanic crust is 5 miles.   three types of rock, igneous, sedimentary, and metamorphic, make up the surface of the earth. that's why 3 option is preferable.