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39 Cards in this Set
- Front
- Back
Reasons for diversity of place names in Africa
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-local terminology
-diverse African languages -external contact -changing political boundaries -colonial history |
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Zimbabwe
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Name was changed from southern Rhodesia, in a deliberate rejection of colonialism
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Cyrenaica
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Roman term for Greek colonies, now part of Libya
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Maghreb
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Arabic for "western lands"
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Africa is the only continent ________ around the equator
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Symmetrical
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Mediterranean zones
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Winter rainfall (North and South)
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Tropical zones
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Summer rainfall (in the center)
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Deserts in Africa
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At 20 degrees North and South (Sahara and Kalahari, respectively)
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Exceptions to why it is difficult to transfer lifestyles between regions
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Along coasts, rivers, Rift Valley in East (summer rainfall crops don't grow well in winter rainfall areas)
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Africa goes from ____ to ____ (latitude
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45 degrees N to 45 degrees S
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Hot air
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-rises
-holds more water (as air heats up, it absorbs water) -expands and rises |
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Cool ait
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-sinks
-loses water -contracts and shrinks |
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Why do climates differ in Africa?
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ITC zones
Monsoons Altitude difference (higher is cooler and drier) |
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Summer rainfall (ITCZ)
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Air directly under sun heats up the most, rises and expands N and S
As it rises and spreads, it cools and loses moisture, which falls to the earth as rain, highest directly under the sun As it spreads north and south it cools so much that it begins to move downward again Dry air moving downwards heats up as it approaches surface, sucking moisture from the land and creating deserts |
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Winter rainfall (Mediterranean)
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Oceans heat and cool less than land.
When land is COLDER than ocean (winter), air moving from ocean to land cools down and loses moisture (rains. Think Seattle! Or, more embarrassingly, Forks?) When land WARMER than ocean (summer), air moving from ocean to land heats up and sucks up moisture (drought) |
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Oceans
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Heat and cool less than land, maintain more constant temperature!
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Cold coastal current
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Such as in Namibia and Peru
Land in tropical regions may never be colder than the sea, so it will rarely or never rain on land. |
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Altitude of Africa
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Much is highland, at about 3000 - 6000 feet above sea level
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Rainshadow desert
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Moist air moving up into mountains cools and loses moisture in rain, then descends on other side.
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Highest rainfall in Africa
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Western slopes of Rwenzoris (Mountains of the Moon) on West side of Great Rift at equator
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What makes it difficult to get up rivers in Africa?
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Major waterfalls and rapids (Nile cataracts, Victoria Falls, etc.) caused by high plateau of interior
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Equatorial glaciers of Africa
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Mt. Kilimanjaro in Tanzania and Mt. Kenya
The advance or retreat of the glaciers tracks temperature and moisture changes |
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Flow of vegetation, going from low altitude to high
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Lowland forest (savanna, to 1km)
Lower montaine forest (to a little bit above 2km) Bamboo zone (if present, from about 2.75km to just above 3km) Upper Montane Forest (from end of lower montane to 4km) Alpine Savanna (4km to limit of vegetation, about 4.5km) |
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Lowland Forest
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Also called Savanna
1km and below Vegetation from 20 to 40m |
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Lower montane Forest
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From 1km to about 2.2km, vegetation from 10 to 20m
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Upper montane forest
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Contains bamboo zone and mossy forest
Vegetation 10km |
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Alpine Savanna
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From 4km to limit of vegetation, about 4.5km, vegetation under 10km
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Five major basins
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they collect sediments and water!
-Niger Delta -Lake Chad -Sudan (the Sudd swamps on the White NIle) -Congo basin (Congo River) -Kalahari (once had a major lake in center, fed by Okavango before tectonics diverted it into Okavango delta and Zambezi riveR) |
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Key to environmental variation
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Moisture availability!
Arid deserts reflecting extreme conditions fo rhuman survival (Sahara) Central African rainforests and distinct fauna Karooo, arid shrubland of South African interior |
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Marine Isotope Stage
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Glacier retreat and expansion linked to climate warming and cooling
Based on framework by Barham & Mitchell (2008) Look at oxygen in the air versus in the sea, get information from sediments. Measure Marine Oxygen Isotope Record |
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Marine Oxygen Isotope Record
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Earth's climate as measured by change in O18 is variable
Measure the O18 versus the O16 trapped in a core. O18 is heavier. When more O18, COLDER period. When more O16, WARMER period. |
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Glacial period
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A colder and drier period, when there is more O18 than O16.
OIS is always EVEN. Contraction of forests, expansion of deserts and grasslands. |
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Interglacial period
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A warmer and wetter period, when more O16 than O18.
OIS is always ODD. Includes the Holocene, which is now. Contraction of deserts and grasslands, and expansion of forests. |
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Oxygen Isotope Stage
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OIS. Arbirary number given to alternating periods of glacial and interglacial
Glacial periods always EVEN, interglacial periods always ODD. |
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Holocene
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The era we're in right now. An interglacial period.
BUT, our forests are shrinking! Deforestation? Global warming? Carbon emissions? |
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Faunal migration
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Possible indicator of climate change. If habitat changes, animals can either go extinct, adapt, or move. Most large mammals move!)
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Archaeological palynology
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Preserved in sediment, fossils, Neandertal teeth, tools
Can get an idea of vegetation that exists in an area, types of soil rainfall, etc. |
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Dating in lake environments
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In lake environment, get animal fossils, nice record of soils and sediments that existed, can do a lot of dating.
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Desert expansions...
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...are recorded in geological record of windblown sands! Kalahari sands lay underneath tropical rainforests!
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