Whois & Analysis for anglerscenter.com

Fishing tackle is the equipment used by fishermen when fishing.

Almost any equipment or gear used for fishing can be called fishing tackle.

Some examples are hooks, lines, sinkers, floats, rods, reels, baits, lures, spears, nets, gaffs, traps, waders and tackle boxes.

Big-game fishing, also known as offshore sportfishing, offshore gamefishing, or blue-water fishing is a form of recreational fishing, targeting large fish such as tuna and marlin which game fisherman regard as having "sporting qualities".

Angling is a method of fishing by means of an "angle" (fish hook).

The hook is usually attached to a fishing line and the line is often attached to a fishing rod.

Fishing rods are usually fitted with a fishing reel that functions as a mechanism for storing, retrieving and paying out the line.

The hook itself can be dressed with lures or bait.

A bite indicator such as a float, and a weight or sinker are sometimes used.

A shore or a shoreline is the fringe of land at the edge of a large body of water, such as an ocean, sea, or lake.

In physical oceanography, a shore is the wider fringe that is geologically modified by the action of the body of water past and present, while the beach is at the edge of the shore, representing the intertidal zone where there is one.

In contrast to a coast, a shore can border any body of water, while the coast must border an ocean; in that sense a coast is a type of shore; however, coast often refers to an area far wider than the shore, often streaching miles into the interior.

Seawater, or salt water, is water from a sea or ocean.

On average, seawater in the world's oceans has a salinity of about 3.5% (35 g/L, or 0.600 M) This means that every kilogram (roughly one litre by volume) of seawater has approximately of dissolved salts (predominantly sodium and chloride ions).

Average density at the surface is 1.025 kg/l.

Seawater is denser than both fresh water and pure water (density 1.0 kg/l at) because the dissolved salts increase the mass by a larger proportion than the volume.

The freezing point of seawater decreases as salt concentration increases.

At typical salinity, it freezes at about.

The coldest seawater ever recorded (in a liquid state) was in 2010, in a stream under an Antarctic glacier, and measured.

Seawater pH is typically limited to a range between 7.5 and 8.4.

However, there is no universally accepted reference pH-scale for seawater and the difference between measurements based on different reference scales may be up to 0.14 units.