Question: The fault lines that led to the creation of the Black Sea contributed to the creation of what other geologic features of Turkey?
About the article "Turkey", section "Geography".

Candidate passages:
Turkey is a transcontinental Eurasian country.
Asian Turkey (made up largely of Anatolia), which includes 97% of the country, is separated from European Turkey by the Bosphorus, the Sea of Marmara, and the Dardanelles.
European Turkey comprises 3% of the country.
The territory of Turkey is more than 1,600 kilometres (1,000 mi) long and 800 km (500 mi) wide, with a roughly rectangular shape.
It lies between latitudes 35° and 43° N, and longitudes 25° and 45° E. Turkey's area, including lakes, occupies 783,562 square kilometres (300,948 sq mi), of which 755,688 square kilometres (291,773 sq mi) are in Southwest Asia and 23,764 square kilometres (9,174 sq mi) in Europe.
Turkey is the world's 37th-largest country in terms of area.
The country is encircled by seas on three sides: the Aegean Sea to the west, the Black Sea to the north and the Mediterranean to the south.
Turkey also contains the Sea of Marmara in the northwest.
The European section of Turkey, East Thrace, forms the borders of Turkey with Greece and Bulgaria.
The Asian part of the country, Anatolia, consists of a high central plateau with narrow coastal plains, between the Köroğlu and Pontic mountain ranges to the north and the Taurus Mountains to the south.
Eastern Turkey has a more mountainous landscape and is home to the sources of rivers such as the Euphrates, Tigris and Aras, and contains Mount Ararat, Turkey's highest point at 5,137 metres (16,854 ft), and Lake Van, the largest lake in the country.
Turkey is divided into seven census regions: Marmara, Aegean, Black Sea, Central Anatolia, Eastern Anatolia, Southeastern Anatolia and the Mediterranean.
The uneven north Anatolian terrain running along the Black Sea resembles a long, narrow belt.
This region comprises approximately one-sixth of Turkey's total land area.
As a general trend, the inland Anatolian plateau becomes increasingly rugged as it progresses eastward.
Turkey's varied landscapes are the product of complex earth movements that have shaped the region over thousands of years and still manifest themselves in fairly frequent earthquakes and occasional volcanic eruptions.
The Bosphorus and the Dardanelles owe their existence to the fault lines running through Turkey that led to the creation of the Black Sea.
There is an earthquake fault line across the north of the country from west to east, along which a major earthquake occurred in 1999.
  Mallory Fault is a natural geologic feature in the Black Mountains near Oatman; ()  
The Levant fault zone is a long transform fault that runs from the northern end of the Red Sea along the Jordan Rift Valley to the Taurus Mountains complex in southern Turkey.
The left-lateral fault zone marks the boundary of the Arabian Plate and the Sinai-Levantine block and has produced pull-apart basins that form the Dead Sea and the Sea of Galilee.
The Levant fault system consists of multiple parallel faults with the dominant features being the Yammouneh and Rachaiya faults.
The fault strand that produced these earthquakes is not precisely known and has been the source of much debate, but the Yammouneh fault has usually been cited as the source for the 1202 and 1759 events. 
Transform faults are commonly found linking segments of mid-oceanic ridges or spreading centers.
These mid-oceanic ridges are where new sea floor is constantly created through the up welling of new basaltic magma.
With new sea floor being pushed and pulled out, the older sea floor slowly slides away from the mid-oceanic ridges toward the continents.
Although separated only by tens of kilometers, this separation between segments of the ridges causes portions of the sea floor to push past each other in opposing directions.
This lateral movement of sea floors past each other is where transform faults are currently active.
Transform faults move differently than a strike-slip fault at the mid-oceanic ridge.
Instead of the ridges moving away from each other, like other strike-slip faults, transform fault ridges will stay in the same fixed location, and the new ocean sea floor being created at the ridges is pushed away from the ridge.
The proof of this is found in paleo-magnetic striping on the sea floor.
A paper written by Gerya theorizes that the creation of the transform faults between the ridges of the mid-oceanic ridge is attributed to rotated and stretched sections of the mid-oceanic ridge.
This occurs over long period of time with the spreading center or ridge slowly deforming from a straight line to a curved line and then finally fracturing along these planes forming transform faults.
As this takes place, the fault changes from a normal fault with extensional stress to a strike slip fault with lateral stress.
In the study done by Bonatti & Crane, peridotite and gabbro rocks were discovered in the edges of the transform ridges.
These rocks are created deep inside the Earth’s mantle and then rapidly exhumed to the surface.
This evidence helps to prove that new sea floor is being created at the mid-oceanic ridges and further supports the theory of plate tectonics.
As previously stated, active transform faults are between two tectonic structures or faults.
Fracture zones represent the previously active transform fault lines, which have since passed the active transform zone and are being pushed toward the continents.
These elevated ridges on the ocean floor can be traced for hundreds of miles and in some cases even from one continent across an ocean to the other continent.
The most prominent examples of the mid-oceanic ridge transform zones are located in Atlantic Ocean between South America and Africa.
Known as the St. Paul, Romanche, Chain, and Ascension fracture zones, these areas have with deep, easily identifiable transform faults and ridges.
Other locations include: the East Pacific Ridge located in the South Eastern Pacific Ocean, which meets up with San Andreas Transform fault to the North.
Transform faults are not limited to oceanic crust and spreading centers; many transform faults are located on continental margins.
The best example is the San Andreas fault on the Pacific coast of the United States.
The San Andreas Fault links the East Pacific Rise off of the West coast of Mexico (Gulf of California) to the Mendocino Triple Junction (Part of the Juan de Fuca plate) located off the coast of the North Western United States making it a ridge-to-transform style transform fault.
The formation of the San Andreas Fault system occurred fairly recently during the Oligocene Period between 34 million and 24 million years ago.
During this period, the Farallon plate, followed by the Pacific plate, collided into the North American plate.
The collision led to the subduction of the Farallon plate underneath the North American plate.
Once the spreading center separating the Pacific and Farallon plate was subducted underneath the North American plate, the San Andreas Continental Transform Fault system was created.
Other examples include:  Middle East's Dead Sea Transform fault  New Zealand's Alpine Fault  Pakistan's Chaman Fault  Turkey's North Anatolian Fault  North America's Queen Charlotte Fault  
Various geological data are rendered as contour maps in structural geology, sedimentology, stratigraphy and economic geology.
Contour maps are used to show the below ground surface of geologic strata, fault surfaces (especially low angle thrust faults) and unconformities.
Isopach maps use isopachs (lines of equal thickness) to illustrate variations in thickness of geologic units.