The present study examined the Northern Shutter Ridge (NSR) that developed along the south eastern segment of the Yagur fault, which extends between Yoqneam and Jalame. This shutter ridge represents a left lateral strike slip movement of about 100 m. An additional 400-500 m left lateral displacement can be deduced from the offset of the first order streams that drain towards it.
A shutter ridge is a barrier formed across a stream-valley by tectonic activity, which blocks the downstream flow (Burbank and Anderson, 2001). The barrier can be formed by vertical (normal or reverse) or lateral displacement. The blocked stream can change its course and flow around the barrier or it can fill the reservoir formed behind the tectonic dam by sediments that accumulate up to the top of the barrier and then overflow it.
In order to examine the possibility of tectonic activity along the Carmel fault, the thick sequence, which was accumulated beyond the shutter ridge, must be explained. It might be argued that this accumulation is not necessarily a result of stream blockage, but it may also reflect a negative balance between water discharge and sediment yield (Low water/sediment ratio) from the drainage basin (Schumm, 1977). Such situation could be related to a climatic deterioration or anthropogenic activity resulted in destroying the forest and intensive slopes erosion. However, in such case a similar sediment accumulation should have been found also in other streams along the Carmel Mt. and so far such accumulation along other streams, is not known.
Two groups of evidence are presented here for young tectonic activity along the Yoqneam-Jalame segment of the Carmel Fault.
The present study show evidence for continuous tectonic activity along the Nesher fault during the Late Pleistocene, but it seems that during the Holocene this branch of the Carmel fault was stable. Tectonic activity also occurred during the Late Pleistocene along the Yoqneam-Jalama segment of the Carmel fault but here there are also indications for Middle to Late Holocene activity.
The tectonic activity represented by the NSR, reflects only part of the left-lateral displacement along the Yagur fault. The amount of lateral displacement at this site is at least 100 m (the length of the shutter ridge), but this amount should be added to the 500 m offset of the southern first order channel of the drainage system that was blocked by the Shutter ridge (Achmon, 1986: Ashkar-Halak, 2009). The offset represented by the three streams that drained toward the shutter ridge seems to decline northward (Fig 2). This change can be attributed to the width of the shear zone in this area (almost 400 m), which raises the possibility that the lateral movement splits between several branches of the Yagur fault.
Three sites were investigated along the Yagur fault in the last years. The depositional history of sediments that accumulated beyond two shutter ridges were analyzed in order to reconstruct their tectonic history, and a paleoseismic study was carried out in a trench excavated across the trace of the Nesher fault, a branch of the Yagur fault (Zilberman et al., 2006, 2009). The young (post Miocene) vertical uplift of Mt. Carmel was investigated in the Nesher Quarry (Zilberman, 2010). The main results of the previous studies are presented below.
The Nesher fault is a short, E-W oriented branch of the Yagur fault, which splits from the main stem south of Nesher. The vertical displacement of this fault declines from 1000 m near the splitting point from the Yagur fault in the east to a few meters in the water divide of Mt. Carmel, some 5 km to the west (Kcartz, 1959). Most of the vertical offset predated the Pliocene (Zilberman et al., 2010), and the young tectonic activity is dominated by a strike-slip movement (Zilberman et al., 2006; 2008).
The Southern Shutter Ridge developed along the N-S oriented segment of the Yagur fault that extends between Yoqneam in the south and the A'amaqim Junction (Jalame) in the north (Ashkar-Halak, 2009). The sequence that was accumulated beyond the barrier was analyzed by Zilberman et al., (2006, 2008). Two periods of sediment accumulation were identified in this sequence: A slow deposition of an alluvial unit rich in weathered pyroclastic fragments (from unknown outcrops of volcanic rocks) started 140±20 ky ago, and terminated before 25 ka, when the barrier was probably breached and the stream incised at least to its present level. This incision was followed by a rapid accumulation of an almost 8 m thick alluvial and colluvial sequence of middle Holocene ( ≥5000 Y.B.P.) age, consisting of eroded soils and carbonate gravels of local origin with no volcanic components. The present incision of the stream in this young fill is younger than 2000 Y.
The Nesher Quarry, exploited by the cement industry, is a submarine channel filled by a sub-horizontal sequence of marine gravity mass-flow sediments. The sequence, more than 60 m thick, was deposited in the margins of the Zevulun Valley during the Messinian and the lower Pliocene at a depth of at least 300 m. It was uplifted to the present altitude (20-90 m) after the lower Pliocene (Zilberman et al., 2010a).
Ashkar-Halak, L., Greenbaum, N., Salamon, A., Zilberman, E., 2006. Morphologic and morphotectonic elements along the eastern and northeastern Carmel Mountain front – evidence for young tectonic activity
. Isr. Geol. Soc. Ann. Meet. Bet Shean, abstract, p. 6.
Braun, Y. (2009). Dating Paleo-seismic Activity on the Carmel Fault Using Damaged Cave Deposits from Denya Cave.
Msc. Thesis Hebrew University of Jerusalem
Braun, Y., et al. (2009). "Dating speleoseismites near the Dead Sea Transform and the Carmel Fault: Clues to coupling of a plate boundary and its branch." Israel Journal of Earth Sciences 58: 257-273.
Shamir, G. (2007). Earthquake epicenter distribution and mechanisms in northern Israel
: Geological Survey of Israel. Report GSI/16/2007. in Hebrew
Zilberman, E., Greenbaum, N., Nahmias, Y., Porat, N., Ashkar, L., (2007). Middle Pleistocene to Holocene Tectonic Activity along the Carmel Fault – Preliminary Results of a Paleoseismic Study
, .Isr. Geol. Surv. Rep. GSI/02/2007, 35 pp.
Zilberman, E., Greenbaum, N., Nahmias, Y., Porat, N., Ashkar, L. (2008). Late Pleistocene to Holocene tectonic activity along the Nesher fault, Mount Carmel, Israel
. Israel J. Earth Sci. 57: 87-100.
Zilberman, Ezra, N. G., Yoav Nahmias, Neomi Porat (2011). The evolution of the Northern Shutter Ridge, Mt. Carmel, and its implications on the tectonic activity along the Yagur fault.
GEOLOGICAL SURVEY OF ISRAEL. Jerusalem, Israel,