CB1 Moderately undulating landscape with slight gilgai (few inches) formation: broad ridge tops and upper slopes of moderately shallow grey cracking clays (Ug5.22 and Ug5.23). Associated are: (i) some dark cracking clays (Ug5.13); (ii) various alkaline (D) soils, such as (Db1.43) and (Dd1.33); and (iii) in the lower-lying situations deeper grey cracking clays (Ug5.25 and Ug5.24) with small areas of (Dy3.43) soils. As mapped, small areas of units HG3 and Kb6 are included in some localities. Occurs on sheet(s): 3,4 CC17 Plains of slightly gilgaied (few inches) cracking clays associated with major and minor functional and nonfunctional drainage-ways: chief soils are grey clays (Ug5.24 and Ug5.25) and brown clays (Ug5.34 and Ug5.35). Associated features and soils are: (i) many small low domes or rises (often levee banks) related to old drainage-ways, with soils of units B10, Si2, and R03 north of about the CollarenebriMoree line (Sheet 3) and of unit Oc12 south of about this line--note that these low domes may give rise to apparent toposequences of soils locally; (ii) small areas of (Dd1.33) and (Dd1.43) soils along the eastern margins of this unit; (iii) some areas of dark clays (Ug5.15 and Ug5.16), especially in the Moree-Narrabri localities (Sheet 3) and possibly related to adjacent elevated basalt areas; (iv) some undescribed (?U) soils on recent terraces and flood-plains along some present streams; (v) some repeatedly flooded areas with grey clays (Ug5.5) having a massive surface; and (vi) some swamps and mar. Occurs on sheet(s): 3,4 CC20 Gently undulating cracking clay plains with moderate to strong (2 4 ft) gilgai microrelief: chief soils are deep grey clays (Ug5.24) with smaller areas of (Ug5.25) and (Ug5.28) and some brown clays (Ug5.34). Soil reaction values of these cracking clays vary and comprise: (i) alkaline or neutral surfaces with acid subsoils (common); (ii) acid throughout (fairly common); and (iii) alkaline throughout (rare). In some areas (Dy2.33) and (Dy2.43) soils occur on the slightly raised flat areas between gilgai depressions or adjacent to small drainage-lines. As mapped, small areas of units B10, MM1, and Ro4 are included in Queensland, and unit Ro1 in the Narrabri area of New South Wales (Sheet 3). Occurs on sheet(s): 3,4 Cb30 Rugged granitic areas with rock walls and tors: chief soils are leached sands (Uc2.3), notably (Uc2.34) and (Uc2.31) with various shallow sand soils such as (Uc4.1) and (Uc1.21). Associated are soils common to unit Wa10 especially in areas of more subdued relief; (Dy3) soils, such as (Dy3.62), often with large amounts of ironstone gravel, especially on undulating ridge tops (?plateau remnants); (Dr2.21) soils on areas of dark intrusive rocks; occasionally soils of unit Rh5; and some of the wetter portions which may approach unit Mw4 in character. KK5 Plateau remnants at high elevation (>4500 ft), rock outcrops: organic loamy soils (Um7.11) in the moister sites with (Um5) or (Gn2) soils in the drier sites. Small area. Data are limited. Kb5 Gently sloping plain of dark cracking clays (Ug5.12) and/or other dark clays such as (Uf5.11) or (Uf6.11). Data are inadequate. Kc2 Dissected basaltic plateau: undulating terrain of dark cracking clays (Ug5.13) and (Ug5.15) in association with (Db3.12) and/or (Dr4.12) soils, often on the stony areas. Data are limited. Kc3 Dissected basaltic plateau--strongly rolling to hilly with some steep, broken slopes, bouldery: chief soils are dark cracking clays, principally (Ug5.13, Ug5.14, and Ug5.15). The associated soils are not known but are likely to include those recorded for unit Kc4 and, less commonly, soils of unit Ms1. Kc4 Dissected basaltic plateau with hills and flat-topped ridges, sometimes bouldery: gently rolling to rolling terrain of dark cracking clays, principally (Ug5.13, Ug5.14, and Ug5.15)and red-brown cracking clays (Ug5.37 and Ug5.38). Associated are (Um6.2), (Db3.12), and (Ug5.12) soils on hills, knolls, and ridges; and small areas of (Gn3.12) and (Gn2.11) soils, especially towards the boundary with unit Mo7. As mapped, areas of unit Kc3 may be included. Kc5
Dissected basaltic plateau with hills and flat-topped ridges, sometimes bouldery: gently rolling to rolling terrain of dark cracking clays, principally (Ug5.13, Ug5.14, Ug5.15), and red-brown cracking clays (Ug5.37 and Ug5.38), some of which may approach (Ug5.6) soils. Associated are (Um6.2), (Db3.12), and (Ug5.12) soils on hills, knolls, and ridges; unit Ms1 soils on ridges, principally the red and yellow earths (Gn2.12) and (Gn2.21), and on slopes, principally the (D) soils such as (Dr2.43); and the (D) soils of unit Ro2 on lower slopes adjacent to that unit. As mapped, areas of unit Kc3 may be included. Kc6 Undulating to hilly with some steep slopes, bouldery in places: chief soils are cracking clays (Ug5.13), (Ug5.15), and (Ug5.3) with red friable earths (Gn3.]2) and sometimes red earths (Gn2.1). Some variations exist between individual occurrences: this unit has similarities with units Kc4 and Mo7. Occurs on sheet(s): 3 Kd4 Valley plains of dark cracking clays (Ug5.15 and Ug5.16). Associated are hillocks and valley side slopes of (Dr2) and (Dy3) soils; and soils locally peculiar to the various adjoining units. As mapped, the size of some areas of this unit tends to be exaggerated. Kh2 Flat to gently undulating plains showing slight (few inches) gilgai features: chief soils are dark cracking clays (Ug5.16) and hard alkaline dark soils (Dd1.33 and Dd1.43) often occurring together as soil complexes. Associated are cracking grey and brown clays (Ug5.2 and Ug5.3); and various (D) soils, such as (Db1.33 and Db1.43). Some deep subsoil and/or D horizon layers may be strongly acid. Kh3 Valley plains of dark cracking clays (Ug5.16) and various alkaline (D) soils, such as (Db1.33), (Dy2.33), and (Dd1.33). LK3 Mountainous--very rugged to steep areas with rock outcrops and sometimes bare rock walls: shallow loamy soils having an A, horizon (Um4.1 and Um4.2) with shallow forms of many (D) soils, such as (Dy3.21), (Dy3.41), and (Dr2.21). As mapped, some areas of units Ub59 and Ub54 are included, and also minor areas of units Kc6 and Rh8. LM1 River terraces and levees: chief soils are loamy soils having an A2 horizon and red pedal subsoils (Um4.31), and yellow-brown earths (Gn2.43) with a general pattern as follows: younger terraces and levees of (Um4.31), (Um6.12), (Um6.11), and (Uf6.3) soils; older terraces and levee slopes of (Gn2.43), (Dr2.42), (Dr2.63), and smaller areas of (Gn2.8) soils. Associated are sand-ridge formations of (Uc1.2), and (Dy2.43) in areas of restricted surface drainage. As mapped, slopes of adjoining hilly country may be included. Occurs on sheet(s): 3 MM3 Flat to gently undulating with slight gilgai (few inches) formation: chief soils are deep cracking clays (Ug5.3), (Ug5.2), and sometimes (Ug5.16). Associated are shallow forms of (Dr2.33) often containing ironstone gravels (see unit Oc20 also). These areas are usually underlain by strongly mottled acid clays. Occurs on sheet(s): 3 Mh7 Plateau remnants at high elevation (>4000 ft)--generally steep slopes with some benches: chief soils are shallow brown friable porous earths (Gn4.31). Associated soils include (Db3.12) and (Dd3.12). Data are limited. Mo7 Dissected basaltic plateau--gently to strongly rolling terrain with hills, knolls, and flat-topped ridges: chief soils are neutral red friable earths (Gn3.12) and structured red clays (Uf6.31), together with various dark cracking clays (Ug5.13, Ug5.14, Ug5.15, Ug5.16) and red-brown cracking clays (Ug5.37, Ug5.38). These soils may cover relatively large individual areas as separate entities or may occur in various soil complexes. Associated are: red earths (Gn2.11) containing ironstone gravels on residuals, sometimes flat-topped, of bauxitized basalt; other red earths (Gn2.14) on rolling terrain and hill slopes, (Um6.2) and (Db3.12) soils on crests and upper slopes of knolls and ridges which are often flanked by cracking clays (Ug5) as recorded above; and minor areas of (Dy3.4) soils. As mapped, small areas of unit Kd4 are included. Occurs on
sheet(s): 3 Ms1 Undulating to hilly with some fairly broad flat areas, often broken by rocky knolls and ridges, some of which may be steep: chief soils are sandy acid yellow earths (Gn2.21), sandy acid and neutral red earths (Gn2.11 and Gn2.12), and shallow sand soils (Uc4.1 and Uc4.2) on the ridges and their slopes where ferruginized rock and ironstone gravels are common. Associated are: flatter and lowerlying areas generally of various hard-setting (D) soils, such as (Db2.32 and Db2.42), (Dy3.41 and Dy3.42); some sandy (D) soils, such as (Dy5.42); some slopes and flatter areas especially in northern expressions of the unit of (Dr2.43) and (Dy3.43) soils sometimes with cracking clays (Ug5); small areas of (Uc5.2) soils; and small areas of soils, such as (Dr4.12), associated with small basaltic flat tops and ridges. As mapped, small areas of units Mz1, Mo5, Kb2, Ke11, and Kc5 may be included. This is a broadly defined and complex unit which may be capable of further division when further data are available. Ob17 Undulating to hilly with some steep ridges, rock outcrops: chief soils are hard alkaline and neutral red soils (Dr2.23 and Dr2.22) with cracking clays, such as (Ug5.13), (Ug5.15), and (Ug5.3); sometimes the (Dr) and (Ug) soils form soil complexes. Associated are a variety of soils including related (Db) and (Dy) soils, and (Dr2.33) soils towards the western and northern limits of the unit. Data are limited. Oc20 Plain--generally slightly raised above the level of the adjacent cracking clay plains: chief soils are shallow forms of hard alkaline red soils (Dr2.33) which usually contain ironstone gravels. Associated are: the (D) soils of unit Ro2; the Ug5 soils of units CB1 and MM3; and some lateritic residuals. Acid clays may underlie these areas There are similarities between this unit and units Oc21 and My3 of south-western Queensland. Qb20 Steep hilly with rock outcrops: chief soils are hard neutral red soils (Dr2.22). Associated are: shallow loams such as (Um4.1) on steeper slopes; (Db1.22) on slopes; some (Uc) and (Um) soils on alluvial fans; and small areas of many other soils including (Gn2.14) on steeper colluvial slopes especially in eastern occurrences of the unit. As mapped, areas of unit Qb19 are included. Qb21 Hilly to steep hilly terrain with rock outcrops: chief soils are hard neutral red soils (Dr2.22) with shallow loamy soils such as (Um4.1). Associated are: (Dr2.21) soils on slopes; (Dy3.4) soils generally on flatter areas and in valleys; (Dr2.4) soils on lower slopes and in valleys; undescribed soils along the narrow stream valleys; and undescribed soils associated with areas of serpentine and associated rock types. Occurs on sheet(s): 3 Qb22 Rolling country: hard neutral red soils (Dr2.22) in association with (Db1.42) and (Dy3.4) soils; other soils including some areas of (Ug5.1) are likely along stream valleys. Ra4 Undulating to low hilly: chief soils are hard neutral brown and red soils (Db1.22) and (Dr2.22). Associated are: (Db1.23) and (Dr2.23) on slopes; (Db1.43), (Dy2.43), and (Dy3.43) in valleys; stony ridge tops of shallow loamy soils, such as (Um4.1) and (Um6.21); and less commonly, (Dr4.12) soils on tops of knolls. Ra5 Hilly with some steep slopes, rock outcrops: chief soils are hard neutral brown and red soils (Db1.22) and (Dr2.22) with shallow loamy soils such as (Um4.1). Associated are small areas of various soils, including (Dy) soils. Rh8 Mountainous--steep often rugged terrain with boulders: chief soils are friable brown soils (Db3.12) with variable areas of (Um6.2), (Ug5.12), and (Ug5.13) soils. Associated are red friable earths (Gn3.12) in areas of relatively gentle relief, and (Dy) soils in some valleys. Data are limited. Ro2 Plains: chief soils are hard alkaline brown soils (Db1.33 and Db1.43) and smaller areas of cracking clays such as (Ug5.15 and Ug5.16). These soils may form soil complexes locally. Associated are: (Dr2.33) on
slightly elevated portions of the plain; (Um6.21) soils on low limestone ridges; and other undescribed soils. Ub56 Low hilly to hilly terrain with some flat to undulating portions, rock outcrops: chief soils are hard neutral yellow mottled soils (Dy3.42). Associated are: (i) a great variety of other (Dy) soils including (Dy3.21) on upper slopes, (Dy3.41 and Dy3.42), both containing ironstone gravels, on relatively poorly drained areas, and (Dy3.43) on relatively low-lying sites and valleys; (ii) yellow earths (Gn2.55) on colluvial slopes; (iii) soils of unit Wa10; (iv) soils of unit JJ6 on hill tops; (v) minor areas of (Dr2) soils on hill slopes; (vi) minor areas (Dg1.41) in wet places; and (vii) minor occurrences of some soils of unit Rh5. Ub59 Hilly: chief soils are hard neutral and acidic yellow and yellow mottled soils (Dy2.42 and Dy2.41) and (Dy3.42 and Dy3.41). Associated are: various shallow soils such as (Um4.1), (Um4.2), (Um6.23), (Dy2.5) on crests and upper slopes; (Dr2.2) soils on upper and mid slopes; and (Dy3.43) and (Dr2.4) soils on lower slopes and flat areas. Ub61 Valley plains: chief soils are hard neutral yellow and yellow mottled soils (Dy2.42) and (Dy3.42) with (Dd1.42) and possibly (Db1.42) and (Dr2.42). Associated are (Um6.11) soils on terraces. Data are limited. Wa10 Undulating to hilly, granitic tors: chief soils seem to be sandy acidic yellow mottled soils (Dy5.41 and/or (Dy5.81); leached sands (Uc2.31) and/or (Uc2.34); and yellow earths such as (Gn2.24) Associated are soils common to unit Ub56; occasionally red earths (Gn2.14); and red earths con taining large amounts of ironstone or bauxitic gravel (Gn2.11). As mapped, areas of units Cb30 and Ub56 are included. There are similarities to units Wa9 and Wa14.