This is a black, sticky stuff. 

Bitumen is a black, sticky stuff. 


Bitumen is a thick, black substance. 

Bitumen comes from tiny living things. Long ago, small plants and animals died in the water. They sank to the bottom of lakes or oceans. Over millions of years, heat and pressure changed them. 
We use bitumen for many things. Most of it is used to build roads. It acts like glue to hold rocks and gravel together. This mix is called asphalt concrete. 
Some bitumen is found in nature. The Pitch Lake in Trinidad is a huge natural deposit. It holds about 10 million tons of bitumen. In Canada, there are also very large oil sands. These sands cover a very big area.
Bitumen is a very thick material found in petroleum. 
This substance forms through a slow, natural way of working. Long ago, tiny living things like algae died in the water. 

People have used bitumen for a very long time. In ancient times, it was used as a cement. The historian Herodotus said it was used in Babylon. It helped build their huge fortification walls.
There are many huge deposits of bitumen on Earth. The Pitch Lake in Trinidad holds about 10 million tons. 

You see bitumen almost every day. Most roads use a mix called asphalt concrete. 

Bitumen is an immensely viscous constituent of petroleum. It is a substance that can appear in different forms depending on its exact composition. It may exist as a sticky, black liquid or as an apparently solid mass. Even when it seems solid, it actually behaves like a liquid over very large time scales. 
The formation of natural bitumen is a slow process involving organic matter. It began during the Carboniferous period when giant swamp forests covered much of the Earth. Tiny living things, such as microscopic algae called diatoms, died and sank to the bottom of oceans or lakes. 

Bitumen has a complex chemical makeup consisting of four main classes of compounds. These include naphthene aromatics, which are partially hydrogenated polycyclic aromatic compounds. It also contains polar aromatics, which are high molecular weight phenols and carboxylic acids. Saturated hydrocarbons are also present, and their percentage affects the softening point of the material. Finally, asphaltenes are high molecular weight phenols and heterocyclic compounds.
There are several distinct types and terms used to describe bitumen. Crude bitumen refers to the naturally occurring version found in the ground. Refined bitumen is the material obtained from the fractional distillation of crude oil. In Canada, the term bitumen is used for extremely heavy crude oil found in the oil sands. There is also "dilbit," which is bitumen diluted with naphtha to help it flow through pipelines. Another term is "syncrude," which is bitumen that has been upgraded to synthetic crude oil.
History shows that humans have used this material for thousands of years. The word "asphalt" comes from the Greek word *asphaltos*, which means bitumen or pitch. Ancient people used it as a cement to join objects together. The historian Herodotus recorded that bitumen was brought to Babylon to build massive fortification walls.
Bitumen is found in massive quantities across the globe. The Pitch Lake in southwest Trinidad is the largest natural deposit, containing an estimated 10 million tons. 
The primary significance of bitumen today is in construction and industry. About 70% of annual bitumen production is used for road construction. It acts as a binder for aggregate particles like gravel to create asphalt concrete. 
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