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EKSIKA JOINT EXAMINATION MAY/JUNE 2016 GEOGRAPHY PAPER 1 312/1 TIME 2¾ MARKING SCHEME 1. (a) it emphasizes distribution of things on the earth’s surface and maps them to show their relationships/pattern 2mks (b) Relief rocks and soil Drainage the earth and the solar Wheatear and climate Natural vegetation any three 3×1 2(b) (i) A – Heave/ Escarpment (ii) B- Upthrow (iii) C – down throw (3mks) b) Vertical faulting across a river may cause waterfall Rift faulting in a enclosed area may lead to formation of a lake if rivers drain into the basin/inland drainage Faulting may influence the flow of rivers e.g rivers may flow a long fault lines/fault guided drainage Uplifting of landscape which leads to faulting may cause rivers to reverse their direction of flow 2×1=2 3.a) Isobar is an imaginary line connecting places with the same air pressure or It is a line on a map connecting places with the same atmospheric pressure b) Recieves reainfal throughout the year 1×1=1 rainfall total between 1000mm-1600mm heavy/high rainfall rainfall occur mainly in the afternoons rain is a companied by thunder there is high humidity double maxima rainfall experiences convectional type of rainfall 4×1=4mks 4. a) Mass waiting refers to the downward/downslope movement of weathered material under the influence of gravity 1×1=1mk (b) Slope The nature of the materials Climate human activities Vegetation Earth movement 5×1=5mks 5. a) sand slone Day stone Silt stone Shale 3×1=3mks 5 (b) New minerals are formed Minerals recrystallize further Rock particles become compacted The physical appearance for rocks change 2×1=2mks SECTION B MAP WORK 6. (i) 1cm rep 0.5km (01KM) 100,000cm =1km 50,000cm 50,000 ×1/100,000 1/50,000 ×100,000 1 1cm rep 0.5km (1mk) (ii) 2021 (iii) 1.6 KM + 0.1 1.5, 1,6KM OR 1.7KM (02mks) (iv)Height of odoido hill 1568m (01km) (i) (ii) 277317 Air photo principal Settlement /huts Tracks/foot path (iii) (02mks) 3mks) Rectangle Space for map Frame 01 Title 01 Features 04 b. iv) (a) Scattered trees, woodland thicket 02mks (b) farming /agriculture-evidence cotton store gu squire 2731 Trading –markets Transport – roads Drainage of the seas 03mks c) the main rivers is river Sio - most of the rivers form dendutic River Sio flows from North East to the western part of the area covered by the map Some rivers disappear further into valleys or swamps Most rivers to the North part of the area covered by the map drain into swamps and any other relevant 4mks 7.(a) Process through which the soil experiences insufficient moisture leading to scarcity vegetation or barren land 02 (b) deserts mostly consist of sand and dust particles that are easily transported and deposited by wind Deserts often are barren hence no vegetation cover in most areas hence wind easily picks the sand and dust Moisture in the desert is insufficient therefore the soil is loosely bind and can easily be picked and transported by wind Most of the deserts are expansive/hence enough space for erosion and fromaioon dunes 3×1=3mks C (i) Deflation hollows Wind blows over the desert surface/landscape and picks the loosened materials like sand through deflation Continuously the materials are removed by rolling and lifting lowering the desert surface Eddy currents caused by the lowered surface continue to erode the depression widening it to form a deflation hollw Space for diagrams 7(a) (ii) it is a crescent shaped mound of sand deposit often found in deserts It develops when sand accumulate on an intervening obstacle that lies in the path of the wind Deposition starts with a small hill with prevailing wind to force some sand to move forward forming a smooth gentle windward slope The effect at the wind eddies cause the formation of steep slope and horns on the leeward side Diagram 7 (d) they are ridge shaped They lie parallel to the path of the prevailing wind Consist of corridors that are between 25-400N wide (e) Strength and speed of wind Intervening obstacles/vegetation Nature of load Water mass/moisture Weather changes Students must explain to score full mark 2× 3=6mks (f) Rock pedestals Mushroom blocks Zeugens Yardangs Deflation hollows Ventifacts Any 2 2×1=2mks (ii) To enable them to attend to all areas of concern To avoid getting lost/losing direction Would help them to estimate the total distance to be covered Helps them to dave time in allocating the features 2×1=2mks 8a. (i) they are thin/shallow They are stony/sandy They are saline are Are usually loose in texture Rich in calcium Have low moisture content 4×1=4 - (ii) nature of the soil/solubility of the minerals topography (b) (i) Parent rock The nature of the rock influences the rate of weathering/ . Hard rock weather slowly while soft rocks weather fast Parent rock determines the soil texture /large grained soil The type of minerals in the parent rock are transferred to the soil during formation 2×1=2mks (ii) topography It determines the rate of weathering/steep slopes encourage high rare of weathering and removal of soil particles It also influences soil depth/gentle slopes have deep soils while steep slopes have thin soils It influences soil drainage/where land is flat, soils are poorly drained 2×1=2mks (iv) Living organisms They assist in breaking down of rocks through burrowing /ploughing /root penetration They influence the mechanical composition of soil by adding /removing organic acid solution/minerals Burrowing / digging /influences soil aerration 8 ( c) A mature soil profile (d) monoculture/farming activities leads to soils exhaustion thus making the soil vulnerable to erosion Overstocking reduces vegetation cover, exposing soil to agents or erosion Ploughing up and sown slopes a slope provides channels for surface runoff. The channels are enlarged to become gullies Clearance of vegetation cover exposes soil to agents for erosion/deforestation Mining/quarrying/road construction loosens/ exposes the soil making it susceptible to erosion Human settlement and cultivation on steep slopes/river frontage/increases soil erosion processes Continuous cultivation without replenishment of soil exhausts it making it vulnerable to erosion Shifting cultivation/bush fallowing leaves hand unprotected against erosion Double tick at the end of the whole explanation 2×4=8mks 9. A(I) Volcanic plugs Acid lava dome Composite conos Geysers/hotsprings Craters Fumaroles and solfatara Lava plateaus and plaind Ash and cindercores 1×3=3mks (ii) through the vents Through fissures Through small cracks /faultiness (b) (i) Collision between tectonic plates (2mks) (ii) faulting/cracking of rocks (iii) Movement of magma within the crust (iv) Adjustment of rocks as a result of stress caused by processes such as folding (v) (vi) Isostatic adjustment. Excessive energy release within the mantle which is explosive Gravitative pressure b.(i) Observation interviewing administering questionnaire photographic/filming sampling c. (i) Acid lava dome ash and cinders hot spring and geysers caldera craters (ii) volcanic eruptions leads to emission of hot ashs and lava that may cause death e.g lava Weathered volcanic materials such as ashes and granite result into infertile soils hence unsuitable for agriculture Some volcanic features create barriers making construction of communication lines difficult and expensive Plugged nature of some volcanic landscapes discourages agriculture an establishment of settlements Volcanic mountains ranges create a rain shadow effect on leeward sides causing acidity e.g in Naro-moru Nyanuki region on the leeward side of mt. Kenya Double tick 4×2=8 (i)the Central coast fo California in N. America around cape town in south Africa Coasta lands of southern Europe Central chile in south America South West and southern Australia 10. (ii) latitude: Temperatures decrease from the equator towards the poles because the sun’s rays fall obliquely on the earth’s surface on the poles. It also influences the seasonal vanation of rainfall 2×4=8 Altitude Temperature decreases with increase in altitude. Reasons with low altitude will have higher temperature than region of high altitudes for every 100m, of ascent, temperature drops by 0.6oC Altitude Temperature decreases with increase in altitude. Regions with low altitude will have higher temperature than region of high altitude for every 100m of ascent, temperature drops by 6oc Distance from the sea Regions located in the interior of continents will have less rainfall and high temperature due to their distances from the sea. Such regions do not benefit from sea maritime air. Coastal configuration This is the alignment, appearance fo nature of the coastline Irregular coastline tend t receive high rainfall because the prevailing winds blow onshare carrying moisture inland Regular coastlines result in less land area coming into contact with the water. Air masses This is large/windspread body of air with uniform properties such as temperature and moisture content. As air mass moves over a region it affects the area it crosses over interms fo temperature and moisture conditions 4×2=8 b.(i) Tropical savanna arid grasslands temperate grassland montane grassland (ii) it consist of tall grass and widely spaced trees Trees are shirt less than 20 metres in height Trees are flat topped and form umbrella shape trees shed their leaves during long dry season most of the trees are Xerophitic c (i) The frequent out break of bush fires that destroys grass retarding its regeneration the increasing human population encroaching into grasslands replacing them with settlements and cultivated land. Frequent drought experienced in the country destroy the grass and the vegetation hence degenerates into a semi desert type 3×2=6mks