The 45 hectare Claypit Nature Reserve  is 33 kilometres east of Narrogin and 7 kilometres west of Wickepin. The reserve appears to be much larger because it surrounds a 5 hectare water reserve, and is surrounded by extensive uncleared land on private properties. The reserve is fenced on east, west and southern sides, but the fence on the west includes a wedge of private bushland in pristine condition. There is no boundary fence on the northern side. Most of the bush is in excellent condition, with relatively few weeds. The entry road splits into a continuing but rougher direct approach, and a more pleasant loop on the left. There are no facilities. Excellent bird watching location.

​​The reserve is a remnant of an ancient undulating upland plain, which separates the Avon and Hotham River catchments.
The multi-million year old plain can be likened to a layer-cake, with a top layer of gravel, sand, or ironstone overlying a pale/mottled/red clay (pallid zone) over decomposing granite or dolerite bedrock. Pallid zone is basically kaolinite clay and quartz grains. A very pure deposit is being mined at Uelelling Hill. It is also the clay in ochres.
A sign adjacent to the Narrogin Kondinin Road is a trifle misleading in associating the reserve with the mafic Binneringie Dyke, which is some kilometres further south. Underlying rock here is mainly granite with a few  intruding dolerite dykes. White granite kaolinite intruded by narrow red kaolinite seams from dolerite dykes can be seen on sides of cuttings as you drive to the water tank.

The ancient plain remnants are gravelly mesas, which are mostly bounded by steep-sided breakaways. Gravelly soil on the mesas has  wildflower-rich often Proteaceae shrubland, which interspersed by wandoo, rock sheoak, and brown mallet woodland.
Hard setting loam and clay soils from the pallid/pink zone on breakaway slopes and upland surroundings downslope are mostly dominated by  Brown Mallet woodland.
 Open Wandoo woodland and more dense Rock Sheoak thickets in and around granite outcrops have more fertile soils formed from basement rock.
​Much of the reserve is fairly easy walking country  but there are no signposted walk trails and people with a poor sense of direction may get lost.

I suggest a visit to the following two areas.

1. WICKEPIN WATER WATER TANK
​Park next to the water tank.

The tank has a capacity of 9 million litres, which is pumped through a pipe from the  Harris River Dam near Collie. Constructed in 1964, the tank is part of a water network that is very important to the district. before this, salinity of land and water sources,which began in the early 1900's caused severe fresh water shortages for people and livestock. Before scheme water, Wickepin residents were dependant on local wells and in desperate circumstances, water from the Wickepin Railway Dam.

​Two informal trails provide access to diverse and wildflower-rich country.
A track winding downhill around the water tank  to a granite outcrop features a range of spring wildflowers. Note impressive Tangled Grevillea clumps. The granite outcrop is on the northern boundary of the reserve. Please avoid treading on delicate lichens in and around the rock.
​Surrounding rocky bushland is choked with dead vegetation and can be difficult to walk through.

An easy walking informal track leads to the breakaway. This is pleasant gravel wildflower country. if you look carefully in land to the west, you may be lucky enough to see some Cowslip/Little PInk Fairy Orchid hybrids. Please leave them intact?- they are precious and uncommon.

2. CLAYPIT
The bare area was an old mining lease to excavate clay for house bricks produced in Narrogin. The red clay overlies a 30 metre wide east-west dolerite dyke, and white from relatively low quartz granite, are also sources of ochre. I collected and made my own red, orange and white ochre from here!
An informal dead-end track on the western side is an easy walk to the west with a breakaway on the left (south) side. The area is pleasant open bushland with some shrub understorey. 

The 100 hectare Yarling Nature Reserve  (36 kilometres east of Narrogin, 7 kilometres west of Wickepin, originally a mallet reserve), is a rarely visited patch of bush. Turn south from Williams Kondinin road on to Watt Road to access the reserve. The view from the road is mostly uninviting due to dense woodland, which hasn't been burnt for decades. This is not a place for the average tourist as there are no trails or facilities, and it is difficult to walk through some areas.
​However, it is an interesting spot with an attractive and wildflower-rich kwongan sand valley on the southern edge.

This area is part of a major watershed, which separates the Hotham, Arthur and Avon River catchments. It contains remnants of an ancient undulating lateritic plain, which has been eroded by river systems to the underlying granite. The millions of years old  plain can be likened to a layer-cake, with the top layer of gravel, sand, or ironstone overlying a pale/mottled clay (pallid zone) over decomposing granite or dolerite.
Like most reserves in the district, Yarling is mostly agriculturally poor laterite or rock. A line of breakaways separate a remnant of the ancient  plain from more recent soils on underlying layers to the north and west.

The northern breakaway roughly follows a dolerite dyke, which is is associated with the Binneringie Dyke further to the south. This is because the dyke was more resistant to erosion from the granite contact line being 'cooked' into more resistant rock, and stony laterite formed on dolerite being more erosion-resistant than that formed on granite.

Much of the sheoak forest is choked by dead saplings, which germinated after a wildfire over 50 years ago, and have slowly died off due to competition without any other fires to remove the dead litter. The shrub understorey has become impoverished because shrubs that depend on fire for germination have died.

A few patches of open Red Morrel woodland occur on dolerite brown loam.

Brrown Mallet whipstick woodland lines the breakaway slopes and edges and other areas where the pallid zone clay layer below the gravel is exposed. The mallets are mostly a uniform size due to mass regrowth after the fire over 50 years ago. Since then the stand has been very slowly thinning in a fairly monotonous landscape.

The ancient lateritic plain on the south eastern side contains lateritic stony and impoverished soils. There are a few stony dryandra ridges and an gentle slope of open Silver Mallet Eucalyptus falcata woodland interspersed with brown mallets. Silver Mallet is a beautiful tree, which can be confused with Salmon Gums. However, Silver Mallet only grows on lateritic gravel soils, and Salmon Gum occurs on clay slopes and valleys.
​
on the southern edge there is group of rare Brown Mallet / Red Morrel hybrids.

Species-rich winter-moist kwongan sandplain on a very broad sandy valley on the southern side contains an a wide range of unusual wildflowers, with varying flowering times from August to November. The lower end is mainly dense Eremaea pauciflora shrubland crossed by numerous kangaroo tracks. From September to November I noticed  plants flowering with the best in late October. The easiest way to reach this area is to walk east from the patch of Red Morrel trees on the western side, but it is not easy walking.

as one walks up the valley Eremaea pauciflora gives way to other species such as Calothamnus quadrifidus and Verticordias on yellow sand then Callitris pines.

A triangle on the south eastern edge was illegally cleared, which is very sad as most of it was wonderful kwongan sandy shrubland of little agricultural value. It was replanted some years later in 1996 to wandoos and understory shrubs. 
The wandoos and shrubs have grown well, apart from the deep white sand area. However after 27 years there are still extensive bare areas and very little recruitment of new species from the adjacent uncleared area.
​Our native bush sandy soils are very sensitive, and recover extremely slowly once organic matter, seeds and native microbes has been reduced.