Geography of Ethiopia Quiz

The Western Highlands are a significant geographic region in Ethiopia, characterized by their relatively low elevation compared to other highland regions, with only a few areas exceeding 2,500 meters.

The Western Highlands are home to various sub-regions with unique features and economic activities. These sub-regions include the Gamo-Konso Highlands, Maji-Korma Highlands, Dawuro-Konta Highlands, Tullu Wallel, and Benishangul mountain.

The Western Highlands are a significant agricultural producer, contributing to coffee, spices, timber, rubber, cattle, honey, and maize. The region also boasts a high percentage of forest cover.

The Western Lowlands in Ethiopia stretch from western Tigray in the north to the southern Gamo and Goffa regions, bordering Sudan and South Sudan.

The Western Lowlands are characterized by an arid or semi-arid climate, with the exception of the Baro-Akobo Lowlands, which experience wetter conditions.

The Western Lowlands are further sub-divided into distinct regions, each with its unique characteristics. These sub-regions include the Tekezze and Angereb Lowlands, Abbay Dinder Lowlands, Baro-Akobo Lowlands, and Omo-Gibe Lowlands.

Due to the harsh climate conditions in much of the Western Lowlands, communities predominantly engage in pastoralism and semi-pastoralism, relying on livestock for their livelihood.

Despite the challenging climate, several towns in the Western Lowlands serve as important business centers along the Ethiopia-Sudan border, facilitating trade and commerce between the communities.

A system of fractures in Earth's crust stretching from the Jordan River valley, through the Red Sea, and across East and Central Africa, ending in Mozambique. It's characterized by volcanic activity, hot springs, and fault lines.

A major geological period that marks the end of the Mesozoic Era. It concluded roughly 66 million years ago.

A process of upward movement of the Earth's crust. Think of the surface rising like a dome or a bulge.

A major part of the Ethiopian Rift Valley System, located in the north, characterized by low altitude, extensive salt plains, and volcanic activity.

A geological feature formed by the sinking of a block of the Earth's crust between two parallel fault lines.

Volcanic cones formed by the accumulation of lava and pyroclastic material.

Depressions formed by the sinking of the Earth's crust along fault lines.

A part of the Ethiopian Rift Valley system located in the central region. It's known for its many lakes.

A geological depression formed by the separation of tectonic plates, characterized by volcanic activity, grabens, and deposition of volcanic material.

A major geological feature in Ethiopia, marked by the presence of several depressions, volcanic mountains, and unique geological formations.

The northernmost part of the Ethiopian Rift Valley, characterized by a unique combination of volcanic activity, grabens, and deposition of volcanic material.

A geological feature within the Afar Triangle characterized by its steep sides and formation through the downward movement of the Earth's crust.

A significant geographical area in Ethiopia encompassing various large lakes and volcanic mountains.

The southernmost part of the Ethiopian Rift Valley, known for its extensive marshy areas and volcanic activity.

A geological feature, often found in rift valleys, formed by the accumulation of sediments deposited by water.

A geological feature in the Chew-Bahir Rift, a mountain range separating the Ganjuli and Galena Valleys.

The state of the atmosphere at a specific time and location, including temperature, rainfall, wind, humidity, and cloud cover.

The long-term average weather patterns of a region, considering temperature, rainfall, wind, and other factors over many years.

Factors that influence the overall climate of a region, such as latitude, altitude, distance from the sea, and the presence of mountains.

Elements that describe the current state of the atmosphere, such as temperature, humidity, wind speed, and precipitation.

The variations in climate that occur across different geographic locations, influenced by factors like latitude, altitude, and proximity to water bodies.

The changes in climate that occur over time, including seasonal changes, long-term trends, and cyclical patterns.

The average weather conditions experienced in a specific region over a long period, often 30 years or more.

The variation in climate from the average conditions, including deviations in temperature, rainfall, and other weather factors.

A zone in Ethiopia characterized by a milder climate than the Dega zone, with reliable rainfall and two growing seasons per year.

The Woina-Dega zone in Ethiopia, with its favorable climate and agricultural potential, is known for its surplus grain production.

The Kolla zone in Ethiopia, characterized by a hot and semi-arid climate, is characterized by altitudes 500-1500 meters above sea level and temperatures between 20°C and 30°C. Rainfall is variable, ranging from 410mm to 820mm, except in the wetter Western lowlands, which receive up to 1600mm.

The Bereha zone in Ethiopia is a hot and arid desert climate found below 500 meters above sea level, receiving less than 400mm of rainfall annually and experiencing temperatures exceeding 30°C.

The term 'Woina Dega' comes after 'Dega' because it refers to a milder version of the Dega zone, with higher rainfall and two growing seasons per year.

The Woina-Dega zone in Ethiopia is a significant contributor to the country's agricultural production, particularly for surplus grain and its derivatives.

The Kolla zone in Ethiopia, with its hot and semi-arid climate, is characterized by variable rainfall, with some areas receiving high amounts due to the proximity to the Western lowlands.

The Bereha zone in Ethiopia, due to its extremely hot and arid climate, presents challenges for growing crops. Its main characteristic is low rainfall and exceptionally high temperatures.

The change in temperature across different seasons in a specific area, caused by the Earth's tilt and the Sun's apparent movement.

The difference between the highest and lowest temperatures in a single day.

The change in rainfall patterns across different locations within a specific area.

The change in rainfall patterns over time within a specific area.

A low-pressure zone formed by converging trade winds, shifting north and south of the equator following the Sun.

A season characterized by clear skies, intense sunlight, and a large difference between daytime and nighttime temperatures.

The Ethiopian region experiencing the hottest temperatures, reaching over 45 degrees Celsius.

The area in Ethiopia characterized by high diurnal temperature range due to clear skies and intense solar radiation.